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                    <text>��I

�\

3

MS

�-

.'•»

BBS Iw

�A
A

university

is

a forum

university

is

a group of buildings.

A
A

university

is

a playground for fun

university

Our

is

for the

exchange

a spirit which spurs

and

of

knowledge.

frolic.

men on

past the limit of endurance to create.

began as Lakehead Technical Institute, blossomed into Lakehead
College of Arts, Science and Technology reaching its pinnacle as Lakehead
University. This task needed men like Dr. H. S. Braun, Dr. W. G. Tamblyn, Sen. N.
M. Paterson and the late Messieurs T. W. Page and P. Ubriaco and others, for the
list is endless. To these men and women Nor'Wester '68 is dedicated.
university

�The Students Are

Pleased To Dedicate

NorWestor

'68

To The Men And Women

Who Gave

Birth

To A

Great And Growing

Institution

IAKEHEAD UNIVERSITY

�4

�..

Expansion

.

.

A

is needed to pour
cement floors on the
upper stories of the Library.

A Bigger Library &amp;
A New Powerhouse

.

crane

the

.

To date the completed Library is
the largest building on campus.

5

�The $14,000,000 Science
complex called the Centennial Building will dominate
the campus when it is completed

in

the spring of 1969.

The heads of the Athletic
Department inspect the interior

of

Building.

the

new

Athletic

LAKE HEAD

UNIVERSITY

�.

.

.

.

A Science Building &amp; A Fieldnouse

The Centennial Building seen here
its

early

stages will

in

take over two

years to build.

The Fieldhouse

just

prior to completion.

.

.

�The University Centre buildthe main stay of stuHoused within its
confines are student offices,
cafeterias, a theatre and a
lounge.
ing

is

dent-life.

The Quadrangle is the original
academic block of the University. It
is
slowly being taken over by the
administrative staff as other facilities
for academics are made available.

A modernistic sculpture by
Gustav Weisman graces the
foyer of the university's newly
completed
$2,500,000
library.

By the fall of 1968 this coeducational residence will be
augmented by a new 240
bed complex. The following
year, a university village will
have been set up with a total
of

480 new beds housed

eight to ten

new

in

three story

�The Campus Today

9

�Students

rooms

meet

for a

gab

in

The phone brings the
dent

their

session.

stu-

Residence in close
contact with those at home
or his friends in town.
in

At the end of these stairs
lies the forbidden zone for

men, Women's Residence.

Relaxing and meeting friends
of

the

lounge.

chief

duties

of

the

is

one

common

��12

�We
.

.

participate
.

are entertained

y

\

mam
* mm

.

.

play

.

.

enjoy ourselves

�We Probe

Individual study cubicles are placed strategicthroughout the library to facilitate study.

ally

Many
the

and

students supplement their lectures from
of materials on the stacks
in the reference room.

ample supply

for

�knowledge

Students may freely browse through
the stacks to find the desired materials.

15

��STUDENT GOVERNMENT

�Message From
The Chancellor

To write a few words for the Nor'Westor,

I

feel gives

me

an

opportunity to give a word of caution to undergraduates and per-

haps the facuty as

well.

One must always remember
to

hold

must be financed and

government and private confidence and backing, each

member must uphold

the dignity and high standard demanded. To

lose the confidence of

government and public

always conduct yourselves
to give

universities

in

is

almost fatal. So,

that honourable high standard needed

Lakehead University your very best

effort.

Senator N. M. Paterson,
Chancellor,

Lakehead University.

18

�SENATOR

N. M.

PATERSON

19

�DR.

20

W. G. TAMBLYN

�Message From
The President
A Yearbook is a
now you

lifelong addition to your personal

memorabilia

.

.

.

Many

pages of this volume,
remembering old faces and special moments that made 1967-68 a memorable
one at Lakehead University. hope that you will recall with pride your academic
and other achievements and will have forgotten the difficulties that might have
been encountered.
would like to thank, on behalf of all the University, the members of the
A.M.S., and the S.A.S., the various clubs and other groups within the University
years from

find yourself glancing at the

will

I

I

meant such a great deal to our general well-being. We are all aware
and effort that is required by these various positions and are deeply

that have

of the time

appreciative of the effort that has been

While
sity

athletic

stands or

falls

and

made

to enrich the University generally.

social activities are vital parts of student

by the vigour and

integrity with

which

life,

the Univer-

members pursue

its

the pursuit of knowledge which unites people of different
and temperaments into the community known as a University.
This spirit of enthusiasm and co-operation has been and will continue to
be a vital factor in the growth and development of our University. It was apparent
this past session in the increased activity of the various clubs and organizations
on campus and the interest in speakers and seminars. This is an indication that
you were eager to pose questions to yourselves and to the political and economic

knowledge.

is

It

capacities, tastes,

our day.

institutions of

To those of you
education elsewhere,

who
it

are graduating this year or leaving to further your

my

is

deepest hope that

the capacity to search for meaningful answers to

we have engendered

you
the questions and problems of
in

today's changing world.
If

there

is

conditions of

and

to

dignity

provide for

and

Ours
in

a single task that should challenge you today,

mankind on

Man

a

earth,

to

liberate

human environment

Man
in

from

is

it

his

which he can

to

improve the

ancient servitudes
truly

manifest

his

practice his freedom.

is

a time of great change, of revolutionary ideas, of

new knowledge

we not bring this new knowledge to solve our greatest
of Man? Should we pioneer in space and be timid on
the bonds of earth and leave man in bondage below?

every discipline. Can

problem

—

"condition''

earth? Must

None

we

we

break

of us have written the script for the condition of

we

mankind today. But

freedom and human dignity, help create in our
day a new condition of mankind, a situation in which human freedom and
dignity are at least possible and not a bitter travesty. Never before in the history of
mankind has this been possible. The vast majority of mankind has ever been
hungry, diseased, ignorant, poor and badly housed. The great glory of science
and all knowledge in our day is that now it provides the means of relieving
this ancient human bondage, these cruel forms of universal human slavery.
can,

if

really believe in

Dr.

W.

G. Tamblyn,

President

Lakehead

21

and Vice-Chancellor,
University.

�Director of Finance

David W. Morgan,
B.A. (AAcGill), AA.B.A. (Harvard)

Dean of Students
John W. Kerr,
B.A., S.T.AA. (AAcGill)

22

�Director of Planning

and

Physical Plant

Claude Smith,
B.A.Sc (Toronto),

23

P.

Eng., M.E.I.C.

��M.S., Ph.D.

Chairman

Board of Governors
John N. Paterson
Vice-Chairman

John Andrews
Murray W. Babe
Henry Bell
Lothar Bode
George L. Carruthers

Robert

J. Flatt

J.

Murray Fleming

E.

Lome Goodall

Donald

F.

Thomas

S.

John

P.

E. J.

Dalzell

Fahlgren

Machan

Donald McMillan
David

I.

Nattress

25

Roderick Philpot

Jones

James

Gordon

lister

Ernest H. Reed

Robert

R.

I

Peden

Hassard

Saul Laskin

Costello

Russell A.

Robert

C. J. Carter
E.

Ernest G. Pa

Peter

J.

P.

Prettie

Ribotto

Bernard Shaffer
Burnley

W. Stevens

�Dr.

M.

E.

Arthur

Professor of History

Dr. H. S.

Braun

Director of

Dr. K. J. Charles
Professor of Economics

University Schools

Dr. F. M. Doart
Professor of Philosophy

Dr. D. G.

i

Dr. T. B. Miller
Professor of History

Frood

Professor of
Physics

Dr. P. Cornell-d'Echert

Professor of
and French

Italian

Dr. J. Hart

Professor of Physics

Dr. E.

L. P.

Mercy

Professor of Geology

m

Dr. J. G. Rideout
Professor of English

Dr. G. O. Rothney
Professor of History

Dr. S.

Walker

Professor of Chemistry

�Dr. A. M. Akram
Associate Professor of

Dr. A. A. D. Asimi
Associate Professor
of Sociology

Psychology

Dr. K.

Dodd

Associate Professor
of History

Dr. D. R. Lindsay
Associate Professor
of Biology and Botany

Dr. E.

Eager

Dr.

Associate Professor
of Political Science

W. Eames

Associate Professor
of

Mr. W. D. Mackinnon
Associate Professor
of Engineering

Mathematics

Dr. C. K.

Meadley

Associate Professor
of

27

Mathematics

Dr. A. Beltran Chen
Associate Professor
of Sociology

Mr. J. W. Haggerty
Associate Professor
of Forestry

Mr. H. North
Associate Professor
of Engineering

�Dr. P. G. K. Panikar
Associate Professor

Dr. A. L. Smith
Associate Professor

of Economics

of English

Mrs. C. J. White
Associate Professor
of Nursing

Dr. P. Barclay
Assistant Professor
of Biology and Botany

Mr. D. Alexander
Assistant Professor of
Business Administration

Mr.

E.

Bauman

Assistant Professor
of Psychology

Dr. J. L. Talbot
Associate Professor

of

Geology

Mr. S. A. Alleyne
Assistant Professor of
Latin &amp; Ancient History

Mr. M. Bjorgo
Assistant Professor
of Library Technology

�Mr. J. Cabot
Assistant Professor
of Economics

Dr. R.

Cowdell

Assistant Professor
of Chemistry

Mr. H. Elmslie
Assistant Professor of
Business Administration

Mr.

W.

R.

Crowe

Mr. D. Crozier
Assistant Professor
of English

Assistant Professor of
Business Administration

Mr.

E.

Mr. M. H. Greenwood
Assistant Professor

Green

Assistant Professor
of

Mathematics

of

29

Anthropology

Mr. P. Coulter
Assistant Professor
of Engineering

Mr. D. C. Dawson
Assistant Professor of

Anthropology

Mr.

C.

Harvais

Assistant Professor
of Biology, Botany

�Dr.

L.

D.

Hawton

Assistant Professor
of Chemistry

Mr. A. T. McEwon
Assistant Professor
of Computer Science

Mrs. A. Moscovitch
Assistant Professor
of

Modern Languages

Mr. F. M. Ishak
Assistant Professor
of English

Mr. D.

J.

McKenzie

Assistant Professor
of Physics

Dr. J. S. Mothersill
Assistant Professor
of Geology

Dr. S. G. A.

Magwood

Assistant Professor
of Biology and Botany

Mr. W. T. Melnyk
Assistant Professor
of Psychology

Mr. G. Mott
Assistant Professor
of Architecture

Dr.

M. Marchand

Assistant Professor
of

Mathematics

Dr. G. Merrill
Assistant Professor
of English

�Dr. D. Orr
Assistant Professor

of Chemistry

Dr. D. S. H. Quon
Assistant Professor

of

Geology

Mr. J. Taylor
Assistant Professor
of English

Mr. C. Ripley
Assistant Professor

Dr. G. Ozborn
Assistant Professor
of Biology, Botany

Dr. P. Sarbadhikari

Mr. D. Sudar

of Philosophy

Assistant Professor
of Political Science

Assistant Professor
of Library Technology

Dr. J. H. Whitfield
Assistant Professor

Dr. J. Whittle
Assistant Professor

of

Mathematics

of

German

Dr. J.

Wilson

Assistant Professor
of Chemistry

Photographs not Available
Dr. V.

Paranjape, Associate Professor of Physics.

Mr. B. Spenceley, Assistant Professor of Physics.

Mr.

T. Griffith,

Assistant Professor, Instrument Room.

Mr. M. Zablocki, Assistant Professor of Business Administration.

31

�FACULTY OF ARTS
Mr. A. Alexander
Mr.
Mrs.

F.

Mr.

L.

Lecturer in English

Anderson
K. Anderson
M. Astwood

Mr. D.

W.

Mr.

Lecturer in Psychology

Alleyne

J.

Mr.

Lecturer in Political Science

Allan

K.

Lecturer in Economics

Campbell
Chimbos
Mr. Min-sun Chen
Mrs.

Leave of Absence
Lecturer in French

J.

Mr.

P.

D.

Mr.

L.

R.

Lecturer in Sociology
Lecturer in History

Teaching Assistant

Clark

Mr. M. Colina

On

Miss M. Dilley
Futhey

Mr.

_

Kozyra

I.

Geography

..Lecturer in

Psychology

Supervisor of Language Laboratory

Hurley

J.

Lecturer in

...Lecturer in English

Mr. V. Gaudino

Miss

Sessional Lecturer
...Teaching Assistant

Teaching Assistant

Leach

...Lecturer in

J.

Mr.

S. R.

Mr.

W.

MacGillivray

A.

McKim

_

On

Mr.

K.

Morrison

Mr.

B.

Phillips

Mr.

P.

Raffo

Mrs. M. Rideout

Mr.

P.

Miss

Shankman

R.

Tracy

Mr.

W. Wahl

Mr.

P.

Mr.

I.

Wesley
Wyschinsky

Mr. G. Yurick
Mr.

E.

Zimmerman

in

English

Economics

Leave of Absence

...Lecturer in

Mr. A. O. Menhart

in Latin

Psychology

in

Mr. D. Lake
Mr.

Spanish

Lecturer in French

Davies

J.

in

Leave of Absence

Mr. G. Courteix

Mr.

Geography

Lecturer

Mr. A. Costanzo

I

in

Lecturer in French

Mr. A. Cloutier

Mr.

Economics

Lecturer in French

On

A. Brigham

J.

in

Lecturer in Russian

Bassil

Miss C. Boissonnealt
Mr.

Psychology

...Lecturer in

Teaching Assistant

Psychology

Lecturer in English
Lecturer

in

Political

Lecturer in

Science

Geography

Lecturer in History

Sessional Lecturer

in

Lecturer

Teaching Assistant

in

in

Spanish
English

Anthropology
Cartographer

Lecturer

in

Psycholgoy

..Sessional Lecturer in Ukrainian

Teaching Assistant

in

English

Lecturer in History

�THE FACULTY OF SCIENCE

On

Mr. W. Allaway
Mrs.

Andrews

K.

Mr.

R.

Mr.

W.

Mr.

L.

Geology Technician
Mathematics
Lecturer in Mathematics
Lecturer in Mathematics

Benett

L.

Lecturer in

Bilyk
D. Black

W. Chu
B. J. Cooke
M. W. Currie
Mr.

Teaching Assistant

Mr.

I.

Mrs.

S.

Teaching Assistant

Dunn

E.

F.

Foldy

Mr.

R.

Freitag

Mr.

L.

D.

Computer Science
Keypunch Operator
Keypunch Operator

Teaching Assistant

Lecturer in Physics
Lecturer in Physics

Teaching Assistant

Mr. D. Isaksson
Mr. D. A. Jones

E. J.

P.

Mr.

B. K.

Mr.

T.

Northcott

Mr.

P.

Skula

Morgan

Mr.

K.

Sumpter

Mr.

R.

W. Taylor

Mr.

L.

P.

Mr.

S.

On

Tullock

W. Watson
Wylynko

in

Physics

in

Physics

Leave of Absence
...Instrument

D.

Mr.

Mr. D.

Teaching Assistant

M. Kendall

Lough
A. Martens
Mountain

Mathematics

...Chemistry Technician

Joshi

W.
Mr. W.
Mr.

in

Teaching Assistant

Mr. D. A. Jackson

Mr.

in

Chemistry Technician

Mr. D. G. Hughes

S.

in Geology
Mathematics

Lecturer

Hansen

Hawton

Mr.

Chemistry

.-Physics Technician

Mr. A. Harding
Mrs. M.

in

in

-

Miss M. Fiorito
Mr.

Chemistry

Biology, Botany Technician

Dowell

Mr. D. Dulley
Mrs.

in

Audio Visual Aids
Teaching Assistant

Davies

Mrs.

Leave of Absence

Biology, Botany Technician

Room

Physics Technician
_.

Chemistry Research Assistant
Chemistry Technician
..Lecturer in Biology,

Teaching Assistant

Botany

Biology, Botany

in

Instrument

Room

Systems Analyst
Teaching Assistant
Lecturer

in

in Chemistry
Mathematics

Computer Centre Manager

�UNIVERSITY SCHOOLS
Mr. H.

J.

Akervall

M. Ballantyne
Mr. A. Bartholomew
Mr. W. N. Bodnar
Mr.

Lecturer

Special Lecturer

P.

L.

..Lecturer in Engineering

_

Lecturer in Engineering

Lecturer in Nursing

Butler

Mrs. M. Coulter

._

Mr. D. C. DeKnock
Dr.

W.

L.

C.

Greer

Sessional Lecturer

Dr.

W. Kembal
Lone

F.

Mr. D. Martin
Mr.

J.

Mrs.

Sessional Lecturer

in

Library Science

Lecturer in Nursing

Sessional Lecturer

in

Engineering Drawing

Special Lecturer

Sessional Lecturer

in

in

Microbiology

Business Administration

Sessional Lecturer

in

Forestry

Murray

Sessional Lecturer

in

Nursing

P.

Mutchler

Mr.

J.

Palko

..Sessional Lecturer in Library Science

Sessional Lecturer

in

Engineering Laboratory

On

Mr. M. Patterson

Sharp

Mr. D.

J.

Mr. C.

Stamp

Mrs. D. Syposz
L.

Nursing

Montieth

E.

Mr.

Mr.

in

Engineering Laboratory Technician

Mrs. N. Kantola

Mr.

Forestry

Anatomy

Lecturer in Forestry

_

Mr. A. Bruley

Miss

in

in

Vidlack

Dr. S. Zingel

Sessional Lecturer

Sessional Lecturer

in

Leave of Absence
in

Library Science

Engineering Drawing
Lecturer in Nursing

Teaching Assistant

in

Forestry

Lecturer in Forestry

34

�Mr. Peter Ubriaco
Mr. Peter Ubriaco, Superintendent of Buildings
died on June 6 at the age of 47.

was

known and very well
and had many friends
among the student body. He showed his sincere
interest and dedication to our University by
Mr. Ubriaco

liked

by

his

establishing

well

associates

in

1965,

the

"Frank

P.

Ubriaco

Memorial Scholarship" with an annual value of
$250 in memory of his father. He also donated
the trophy awarded annually to the Lakehead
University Squash champion, and a painting
which now hangs in the library building.
Mr. Ubriaco was an employee of the University
for

a period of three years.

—Argus, June

29, 1967.

�Alma Mater
Society

William G. Weiler,
A.M.S. President

Message

President's

—

The 1967-68 year at Lakehead has proven one thing without a doubt the
is growing up! And with this period of maturation, we have experienced inevitable growing pains. Never before in our short history have so many
students become involved in student government. Never before have they stood
up and questioned their rights, their positions, and their obligations.
University

In

many ways

it

was

a year of unrest. But out of this has grown a more

powerful student awareness and surely
active interest in student
This past year

government

we have

in

pattern will lead to an even

this

more

years to come.

seen a tremendous change

in

attitude of students

towards academics, probably best emphasized by the increased demand on our
library facilities. With Lakehead University's coming of age, the veil of 'a
glorified highschool'
It

is

finally being shed.

has been a pleasure and an enlightenment for

of Lakehead University

and greater things

to

in

'67-'68

come

and

I

me

to serve the students

wish the new executive continued progress

for the '68-'69 year.

36

�37

�—

Alma Mater Society Council
TO

—
—
Murray —

—

—

President, Mike Barkwell
Secretary, Bill Weiler
Chief Justice.
Arts Rep.,
2ND ROW: Marilyn
Nursing Rep., Don Cordingly
Arts Rep., Julie Wierzbicki
Arts Rep.,
George Paddington
University Schools President, Fred Poulter
Science Rep., John Sihvonen
Pia Saccu
Nursing Rep.
Nursing Rep., Gerald Mosa
University Schools Rep., Marg Fleming
BACK ROW: Don Bergman Science President, Dave Parsons Arts Rep., Greg Cox University Schools
L.

R.

SITTING: Don Lees

Vice-President, Bert

—

—

—
MISSING: Bob Wynn —
Rep.,

Doug Curtola

Treasurer, Joan Stuart

Bauman

—

University

—
—
—

—

Schools

Rep.,

Peter

McCormack

President.

University Schools Rep., Rick

Middaugh

38

—

—

—

Arts

Rep.,

Science Rep.

—
—

—

Pentti

—

Paularinne

Arts

�EXECUTIVE: Mary Rekszynski
Kathy Buie
Treasurer.

—

—

Secretary,

Pentti

Paularinne

—

President,

Tom Goodman

—

Vice-President,

Arts Society

COUNCIL: SATING: Bill Gartrell, Mary Rekszynski, Pentti Paularinne, Tom Goodman, Kathy
STANDING. Ken Robinson, Beth Hagglund, Harvey Clue, Kalid Ali, Tracey Hanna, Pat O'Brien.
MISSING: Gary Kunnas, Penny Connor.

Buie.

�Science Society
EXECUTIVE: Garry Kinoshita
Bergman
President,
Glen

—

President, Fred Poulter

University Schools

Society
EXECUTIVE:

Debby Bryant

George

—

—

Paddington
President,
Dave Roden Vice-

Secretary,

President.

MISSING: Fred Wilmot

—

—

Treasurer.

40

—

—

Secretary,

McLeod

Treasurer.

—

Don
Vice-

�THE FOUR SEASONS

�mouths were

dry.
All those in attendance enjoyed the meal put on by Mr.

Gude and

his staff.

Gay

conversation

and good booze.
42

�Some people
how to enjoy

really

know

themselves.

�.

.

8. S. S.

Presents

"F

Myrna and Chuck Tracy

The Freemen

a folk sing

.

.

The Summer School Society in conjuncwith the Lakehead Folk Guild gave
the summer school students an enjoyable
evening of folk singing. Such songsters as
Myrna, The Freemen, Chuck Tracy and
tion

Andy Washwell made the
treat. But that was not all
.

night quite a
.

.

1

.

.

�.

.

and a wiener roast

��Frosh Queen

FROSH PRINCESS

FROSH PRINCESS

Miss Eeva Suvanto
University Schools

Miss Susan Haglund
Faculty of Arts

Victory

Kiss

from George,

President
Schools.

\

47

Ah

of University

��Week was the Faculty Parties. The Faculty of
Mount McKay Ski Area while the Faculty of
Science and the University Schools combined and held their s at Chippewa Park.
The main event of the evening for the Arts' students was the free ride up the
One

Arts

chair

of the highlights of Frosh

held their function at the

lift

to take in the panoramic view of the city lights by
by folk singers and a dance also was on the agenda for

which enabled them

night. Entertainment

the Artsmen.

Meanwhile

at

Chippewa Park

students were treating themselves to a dance

and University School
wonders of the location.

the Science

and

to the

�50

�Her Skating
Party

Two

of the

many

events held during Frosh

were the Volkswagen Push and
Party.

the

Roller

Week

Skating

Proceedings started with the contestants and

meeting at the university. The Faculties
pushed their VW's from the U to the Fort William
Gardens where the roller skating was held. University
Schools made up of almost totally Foresters won the
push over Science, with Arts defaulting.

their

Where's the opponents?

cars

�Frosh Week Kangaroo

�Wind-up Dance

Kourt

if
The Gettysbyrg Address

Kangaroo Kourt and the Frosh Week Windup Dance brought to an end a great week.
Such punishments as eating a cream pie while
both participants, the one being fed and the
feeder were blind-folded; or sewing a patch
on blue jeans while a poor frosh was in them
were handed out to the first year students by
their big brothers.

On

The

the last day, The Gettysbyrg Address

entertained.

Honest! I'm flat chested.

jury here-by

53

-

�The Treasure Van, sponsored by W.U.S. brought
world-wide selection of articles.
variety of items, from interesting ornaments to

to the University a

A

somewhat
a shopper.

different practical articles attracted

many

�55

�"We had some

chickens,

no eggs would they iay

."
.

.

56

�The Arts Society Presents

.

.

�All entertainers

Andy Washwell

were present

except the Travellers

for the first

number.

�The Ramblers is a group which
performs especially for the Folk
Spectacular. They combined folk
and western to be one of the
most popular groups present.

The

Freeman entertain while the
cast watches from the

rest of the

background.

George and Myrna. Myrna

thrilled

the

audience with her rendition of "White
Rabbit".

Frank Shoemaker

f

w4

i
59

�Nemissa

V
99

Campus
The

social

club

was a time

Cuties Caper

evening held by Nemissa, the University's
of entertainment

and

girls'

relaxation for the female

was highlighted by a fashion show and
much enjoyed skits. It provided the opportunity for the
girls on campus to become better acquainted with one another.
students. The evening

the

'Say

it

with flowers"

Florine's discourse

way

60

life is.

on the

�ircle

K
»9

'The White Rabbit Bail
Circle "K" once more made a success of the
annual Hallowe'en dance. A variety of costumes,

eerie atmosphere,

music

all

spooky

to

that haunting flavour of a

night.

Am

61

added

appropriate decorations and

I

in

the

wrong place?

��The Ortona Legion was the scene of the
Annual Alma Mater Society Dinner
Dance. Guest Speaker, Dr. T. Miller spoke
in great depth on "University Government".
With his speech Dr. Miller brought waves
First

of laughter from his listeners. The meal, a

smorgasbord and the music of Moe
rounded out a superb evening.

—Guest Speaker

Dr. T. Miller

!

63

I

Ktytor

�The top of Mount MacKay provides the
photographer
ample opportunity to
photograph the city below.

This

adventuresome group of individuals

climbed to the top of Mount MacKay. This
outing is fast becoming an annual event.
The majority of those participating are from
Residence and the Forestry Faculty.

64

��66

�Blood Donor Clinic

���The

New

Year's Kiss

�Out went the old and

in came the new, 1968,
To commemorate the occasion
and guests were feated to a gala
extravaganza. Imaginative decorations, the music

the new
students

year.

of the Beltones, two go-go girls and a delicious
buffet dinner all helped to bring in the New Year.

A shower
greeted the

of balloons
New Year.

�eager and keen University
U at 6:00 a.m. on a frosty January morning. And each team has in its possession a
tandem bicycle.
Picture one team pulling off their rear wheel minutes
before the race; it seized on them.
Picture another team with gear sprockets that spread
apart so that the gears were useless
And still another bunch of students with a front tire
with no less than three bulges on it. Their rear sprocket
seven

Picture

teams

of

students, gathered at the

.

.

.

broke at a crucial point of the race.
All

this

was

part of the

Pre-Carnival

festivities.

The

190 mile bicycle ride (attempting to reach the University
campus) was an effort in cementing

of Minnesota Duluth
relations

know

between the two campuses and

letting

U.M.D.

of our Carnival activities.

Mother nature had other ideas and blanketed the route
six inches of snow.
Although the cyclists reached only the half way mark
all agreed it was quite an experience.

with over

72

�73

��Arts Dinner Dance

�President W. G. Tamblyn, Rev. Father Bauer, and Chairof the Board of Governors, Dr. M. W. Bartley.

man

Rev. Father D. Bauer, guest speaker.

Athletic

Trophy Night
Susan Savage, top
female athlete of the
year accepts congratulations from
Dr.

G. Merrill.

�The Athletic Trophy Dance, one of the next to last
was the evening set aside to
honour the sportsmanship and success of participants
social events of the year,

in

both

inter-collegiate

and intramural

sports.

Rev.

Father David Bauer, Advisor to the Canadian National

Hockey Team and lecturer at St. Mark's College, opened the presentation of trophies with a speech on
athletics

being an important factor

in

shaping well

adjusted individuals.

Coach Birger and Mrs.

J.

DuSang

of the Athletic Department.

Don Holmstrom was chosen
Male Athlete of the Year
due to his superb year in
Inter-Collegiate

77

Basketball.

�C. J.

Sanders

Athletic Building

Opens

78

�79

�on stage ...

Ian

&amp; Sylvia

To relieve pre-exam tensions, nearly 2,000 students turned out to see Ian and Sylvia in the C. J.

Sanders Athletic Building. They were well entertained by a variety of vocal and instrumental tunes
by the versatile duo.

80

�81

��Chad Hannah

Joe Fraser

Ken Conrad

Gord Fukushima

Larry Hebert

Jim Purdon

THE ARGUS

VOLUME

II,

The Argus
The

University.

Session

No. I-XXII
is

published weekly by the

opinions

expressed

are

Alma Mater

those

of

the

Society

1967-68
of

not necessarily those of the A. M.S. or the Administration. The

ARGUS

Lakehead

board

editorial
is

and

authorized

second class mail by the Post Office, Ottawa for payment in cash. All correspondence to the ARGUS main office behind the lower cafeteria; mail c/o

Lakehead
editor

associate

managing
features

news

University, Port Arthur.

chuck grieve

bob

sports

advertising

leggett

chad hannah
boyd hussey

circulation

supplement

joe fraser

83

larry hebert

jim

purdon

gord fukushima
ken conrad

�Photo Directorate
To meet the growing needs of
both the Nor'Wester and the Argus,

equipment and men were pooled

to

form the Photo Directorate. Working
out of one central base the Photo
Directorate

photographed events

for

both Lakehead University Publications

and any other campus organization
which needed the Photo Directorate's
services.

Under the

direction of Jed

Drew,

Photo Director and Jim Zatulsky,
Assistant Photo Director, the staff
of the Photo Directorate

commended

is

to

be

for a job well done, as

exemplified by the photographs seen

throughout Nor'Wester

—Jed Drew

Photo Director-

84

'68.

��King Carnival, Dave Parsons, drinks one of his
prizes, a yard of ale.

Those present at the Bushmen's

Ball

had a preview

86

of the Princes

and

Princesses.

�King Carnival
crowned

at

Bushmen's

Miss Dominion of Canada
crowns King Carnival with
a carnival toque.

Miss Winter Carnival
1967 congratulates
Dave Parsons upon
being chosen King.

The Quiet Jungle
entertain.

��Bob Gude,
caterer of
the dinner
helps a
staff

member.

Tours of the University and a
buffet dinner were the order of
the day on Sunday of Carnival
Week. Foods from many countries
of the world were featured for
all present. Booths decorated to
national
setting
simulate
a
varied from a Chinese Tea House
to a

Dutch Windmill.

International Dinner

�The Faculty of
Arts again takes
first

place

in

the

sculptures.

Snow

��92

�The Noblemen

93

��then the

Wine &amp; Cheese
Party...

and to recuperate

Back Rubs

95

�The Faculty of
Engineering took
the theme of
their float

from

the recent

Disney film,
Jungle Book.

Parade

Snow White and
ed

first

the Seven Dwarfs captur-

prize for the Nursing Faculty.

96

��Just because I've got a dress on doesn't
I'm a girl!

mean

���TorchLight

Parade

A

group of over seven hundred students filled
paraded through the streets of downtown
Port Arthur. Although darkness was supposed to prevail
the combined light of their torches caused the sensation
of its being mid-day. The parade was culminated in a
huge, though slightly illegal bonfire.
with

101

spirited
spirit

�102

�Gordon
Lightfoot
in

concert

�Chinese students perform
the Dance of the Porcelain

Charlie and Bill sing American Folk Songs.

Spoons

Art's Society's International
Students

from

about

their

Africa

tell

homeland

through song.

The Estonian Dancers

�The Arts Society's International
Night was one of the many features of Winter Carnival 1968. As
the title of the evening suggests
the night had a flavour of the international to it. Featured were
most of the countries of the world
which have students attending
EntertainLakehead University.
ment varied, from Americans sing-

ing folk songs to Oriental students
performing the Chinese Dance of
the Porcelain Spoons.
During the intermission the candidates for the title of Miss Winter
Carnival were judged in formal
gowns. Miss Dominion of Canada

was one

of the judges.

Entertainers from the

Tom

West

Indies

Kelly sings to the future Miss Winter
(left) and to the first runner-up.

Carnival

��Winter Carnival Finale

The singer with
the AAcLintock
orchestra.

Decorations depicting the Wide Wonderful World of Colour, the
Disney theme of the Winter Carnival set the spirit for the grand formal ball held at the Port Arthur Armoury. Entertainment was supplied by Ellis AAcLintock and his 17 piece orchestra. Highlight of the
evening was the selection of AAiss Heather Laing, representing the
Faculty of Forestry as AAiss Winter Carnival 1968. Miss Nina Quinn
of the Faculty of Business Administration was chosen as first runnerup and Miss Sue Laban of the Faculty of Science as second runnerup.

107

�MISS WINTER CARNIVAL
Heather Laing
108

�Miss Business Admin
Nina Quinn

Miss Science

Sue Laban

�Miss Arts

Susan Hagiund

Miss Ryerson Tech.

Mary-Lou DiGiacomo

��Miss Dominion
of Canada

on Campus

Tom

Kelly serenades Miss

Dominion of Canada

at Inter-

national Night.

i

��Art Club
John Howard,
Vicki Smith,

Brooke Hill,,
Gerald AAosa, Peter
AAcCormack, Charlene
Fitzpatrick.

Biology Club
Bryan Probizanski —
—
Gary
—
Fawn
—

President,
Fred Poulter
Vice-President,
Kinoshita
Treasurer,
Elsey
Secretary.

Business Club
Linda Cole

—

Secretary,

—
—
—

Jeff Shivrattan

President,

Lawrence Vice-President,
Bob Katajamaki Treasurer.
lain

�Circle K
Michael Pawlowske
Secreta ry-Treasurer,
Jerrald Burns
President,

—

Robert Yatkowsky
Vice-President.

Chemistry Club

—
—
—
Jouni
Heckley —
Ross

Chuchman

John McLeod
Kraft

Paul

Secretary,
Vice-President,
Treasurer,
President.

Chinese Students'

Association
Joe-Chuen Frank Yam —
David Lee —
Edward Chan —
Bernadette Ng —

Treasurer,

President,

Vice-President,
Secretary.

�C. U. S. 0.

—
—
—
—
—

Val Dennison
President,
Linda Martin
Secretary,
Mr. Cloutier
Faculty
Advisor,
Jeannetty Gall
Chairman,
MISSING— Charlene
Fitzpatrick

Conservative Club
—
Bryan Mclver — Vice
Mary Greer — Treasurer-Secretary.
Bill

Bartley

President,

President,

Engineering Society
Doug

Curtola

—
—

President,

Margaret Burns

—

MISSING

Secretary -Treasurer,
Vice Pesident.
Terry Henry

116

—

P. R.

�—

French Club

—
—
Melnychuk-—
Mary Mercy —

Jean Boyes

Vice-President,
President,
Luella
Treasurer,
Secretary.
MISSING: Paul Paularine, P.R.

Don Murphy

Inter-Varsity
Christian Fellowship
FRONT: Bonnie Wile, Jean Jones.
BACK: Vicki Smith, John Howard,
Jim Ferguson, Jo-anne Cain,
Vivian Nyyssonen.

.i

n

nJ""&gt;-

Sii
Liberal Club

—
—Second
—
Gammage —
Standing: Linda Martin —
Bryan Springgay —

Jeanetty Gall

Bob Gibson
Fred Porter
Keith

Secretary,
Vice-President,

President,
P.R.,

Treasurer,
Past President.

MISSING: Larry Eustace
First

Vice-President.

�Library

Faculty

—

Debby Bryant University Schools Rep.,
Brian Harrington
Secretary Treasurer,
Michael Gravelle
Vice-President,
Charlotte Elwert
President,

—
—
—
Barb Williams —

Councillor.

L. U. F.

—

A.

Moes Secretary, Bob Wynn
Vice-President, Don Smith
Public
Relations. MISSING: George Munroe
President, Paul McAllister
Treasurer.
Alida

New Democratic
Ward Olson

—

Robinson

President,

—
—

Treasurer, Ken

Harvey

Vice-President,
Secretary.
Evelyn Ste. Croix

Lenetski

—

—
—

�Nemis
Sandra Knight—
Kidd —
—

President,
Vice-President,
Suskila Lalsingh
Secretary-Treasurer.
Irene

Nursing Association

—

Sharon Weller Treasurer, Lynn
Lehto
2nd year rep., Kathy Galvin
Recording Secretary, Linda Thomas-

—

President.

Ukrainian Club
Gerald Mosa —
President,

—

Stephanie Boyko
Secretary,
Roman Stavanczak Treasurer
AAark Slotiuk

—

—

Vice-Presider,1.

�Vietnam Action

Committee
FRONT ROW: Evelyn Ste. Croix,
Lome Seaman Chairman,
Ward Olson, Harvey Lenetski.
BACK ROW: Ron Pappin, Bill

—

Walker, John

Scott.

West Indian
Association
—
Jean
Khalid
Javid
Jones —
Naqvi —
President,
Secretary,
Treasurer.

Ali

Winter Carnival

Committee
—Chairman, Heather Laing —Co
Bob Katajamki—
—
MISSING: Wendy

John Lee

ordinator,

Ticknor

Treasurer.
Co-ordinator.

���123

�124

��*

1

����S. A. S.

President's

Message

Glenn A. Miller
President

Rapid expansion of enrollment and
past three years has resulted

grams

in

in

facilities at Lakehead University over the
tremendous acceleration of extra-curricular pro-

both academically and athletically oriented

counterparts necessary

in

creating

activities.

and maintaining a strong

These are the

University

spirit.

The true campus atmosphere can only be achieved where there is a balance,
which varies with the individual student, between academics and athletics. It is
the object of the Student Athletic Society to provide, promote and administer
the athletic program needed for this balance.
I

would

like to

take this opportunity on behaiLof the S.A.S. Executive and

Council to thank Mr. George Birger, Mr. Henry Akervall, Mr. William Shannon,
and Mrs. Jutta Dusang from the Athletic Department for the time and effort they

gave

to the S.A.S.

and

to the students.

was made

one of the most extensive and diversified
athletic programs ever offered at Lakehead University. A program comparable to
those at any larger Canadian University. It was only the unforeseen delay in the
completion of the gymnasium complex that prevented the entire planned program
This year, provision

for

from becoming operational.
The

staff,

the facilities,

and the program are established now.

Next year, for those of you returning, an excellent Athletic Program
be operational. My sincerest wish is that you will use and enjoy it.
Glenn A.

Miller,

S.A.S. President.

130

will

�S. A. S.

Executive
L.

Gander

—

Treasurer, W. MarosticaPresident,

Secretary, G. Miller

—

D. Battiston.

S. A.

S

Council
1ST

ROW:

Gander, G.

A. Holt, N. Sackett,

Marostica, M. Broadhurst, Z.
chelak.

L.

W.
Ma-

Miller, D. Battiston,

2ND ROW:

L.

Albertini,

T.

Comishin, M. Siemieniuk, S. Savage, P. McAllister, J. Buie, D.
Goodman. 3RD ROW: A. Johnson,

C

Montgomery,

mer,

G.

Magee, G.

131

J.

Skinner.
Barr,

J.

Jasiura,

4TH

B. Bry-

ROW:

North.

D.

�Athletic

Department
Administration

Mr. G. Birger
Director of Athletics

Mr. W. Shannon
Co-ordinator of Athletic Activities

Mr. H. Akervall
Director of Intermural Athletics

132

��134

��FRONT ROW:
C.

P.

Battiston, D.

M. Smith,

B.

Lenardon,

Laliberte.

Crocker,

D. Ostaff, D. Olinik.

R.

Manager;

BACK ROW:
Tapak,

D.

K.

Kivisto,

J.

Stefiszyn,

Siciliano,

D.

K.

Miyata,

B.

Hussey,

R.

Gellert,

B.

Magee; Manager. MISSING: A. Johnson,

L.

H. Akervall, Coach;

D.

Nutall,

J.

Fallis,

J.

Wilkie,

Grogan,
Gander,

�Intercollegiate
Clair Battiston helped make up the Nor'
Westers strong defensive core.

Hockey
The end of the regular season of the International
Collegiate Hockey Association saw the championship
eluding the defending champions the L.U. Nor'
Westers. The championship went to the new entry
in the league from Lake Superior State College, the
Soo Lakers. The Nor'Westers came out of the season
with the distinction of being the only team to defeat
the new champions. Added to this Murray Smith,
second leading scorer in the league secured a spot as
a winger on the I.C.H.A. All Star team.

137

�The

final score.

World Hockey
Action

Stops like this one by Bamford stopped the Rumanians cold in their
tracks.

�For the

hockey

first

time ever a Lakehead University varsity
opposition from an International

team faced

calibre team.

One

of the

up and coming teams

hockey, the Rumanian Nationals posed a
to the Nor'Westers. The threat was met
The University squad with a few T.B.H.A.
including Coach Akervall downed the
the score of 7-3.

Kilgour was the light that sparked
the Nor'Westers to victory.
Stefiszyn

is

foiled again.

in

world

great challenge
and put down.
Senior pick-ups

Rumanians by

�Intercollegiate

Squash
The Lakehead University Squash team of Bruce Brymer,
Jerry Kishi, Glenn Miller, John Sihvonen, and Coach Dr.
G. Ozburn placed second to Osgoode Hall Law School
in the Ontario Intercollegiate Championship in Toronto.
Each of the members of the squash team played three
matches and each lost one for a total of eight points.
York University placed third with six points.

Glen Miller

140

�O.I.A.A. CHAMPIONS: FRONT: Tony Marsonet,
Coach; Dick Battison, Dave Kerr.

Bill

Hodgson. STANDING:

Rod Ferguson,

Bill

Shannon,

Intercollegiate

Golf
Lakehead University won the Ontario Intercollegiate Athletic Association Golf
Championship in Hamilton. The tournament was a 36 hole, ten team event hosted
by Mohawk College. Each of the ten Universities competing named four golfers
to their team, the lowest score of the four man teams to be declared the winner.
The Lakehead University team was made up of Tony Marsonet, Rod Ferguson, Bill
Hodgson, Dick Battison and alternate Dave Kerr. Tony Marsonet was the low gross
golfer on the Nor'Wester team and was only second to a golfer from Waterloo
Lutheran University. Tony shot 76-80 on the par 71 Mt. Hope Golf Course. Rod
Ferguson had a 160 total with rounds of 80-80. Dick Battison and Bill Hodgson
followed Rod Ferguson to round out the Lakehead University total of 646 strokes.

141

�FRONT: Arnie Anzew, Larry Hebert, Roy Holman, Rob Cameron, Rob Woods, George Kostyshyn.
BACK: Hugh Cameron, mgr., Jim Johnston, Bill Horychuk, Don Holmstrom, Lou Pero, Lloyd Koski,
George Birger, Coach. MISSING: Moe Siemieniuk, Peter Andros, Gordon Walford, mgr.

Men's Nor'Wester Basketball

�Short in height, but long on abilithe Nor'Westers won 13 of

ty,

—

24 games this year
their
under Coach George Birger.
Don Holmstrom set a university
record by scoring the 1000th
point of his Nor'Wester career.
An even better season is hoped
for next year since all the players are expected back.
their

first

143

�O.I.A.A.

CHAMPIONS: Gary Kunnas, Mike Wren,

Brian

Nelson,

Larry

Freeman,

Dave Dobbin, Tim

Hanrahan.

Intercollegiate

Skiing
row LU.'s Nor'Wester Ski team captured the Ontario
Championship. The team was composed of Mike Wren,
Larry Freeman, Gary Kunnas, Dave Dobbin, Brian Nelson and Tim Hanrahan and
was coached by Bob Morgan and Tom Morton. The championship was won by a
30 point margin over Northern College with Osgoode Hall in third place. A total
of nine other colleges and universities participated in the meet held at the
For the second year in a

Athletic Association Ski

Levack Ski
In

the

Hills in

first

Sudbury.

race, the Slalom, L.U. placed

first,

six

points

ahead

of Trent Uni-

Second race, the Giant Slalom was a complete reversal for the
Lakehead team. They had a disastrous second run to place seventh in the race
and second in the Alpine Combined behind Trent. The team placed second to
Northern in Cross Country. Dobbin and Wren took the Jumping 1-2 to win the
championship for the Nor'Westers.
versity but the

144

�Curling

The Lakehead University Curling team skipped by
Andrusco, with L. Eustace Lead, C. Montgomery
Second and T. Fry at Third, placed third in the O.I. A. A.
B.

Curling Championship at the Terrace Curling Rink in
Toronto against several other university teams.
The Andrusco Rink was also intramural champions
at L.U. with second place going to the rink skipped

by Dave Home.

145

��Pictured
of

tatives

offered

above are represensome of the sports

this

year

at

L.U.

Left:

Dave Montgomery and other
versity

students

Lakehead

Mustangs

campus

lack of a

BELOW

play

uni-

for

due

to

the
a

football team.

AND

RIGHT: The
Rag-Tag Football
Champions. BELOW RIGHT: Two
fine outdoor tennis courts have
been built for those who are inLEFT

Foresters,

terested

in

that sport.

147

�Mrs. J. DuSang
rhythmic gymnastics
instructress, above,
demonstrates techniques
used in the

practice of

rhythmic gymnastics.

Rhythmic gymnastics
movement executed

is

in

time, space, energy,

and form. Every motion
expressable by a movement, every movement
creates an impression
as exemplified by the
above left and centre

photographs.
Mrs. Irwin, fencing
instructress,

below gives

instruction

to a novice

fencer.

148

��Faculty of Arts

G. O. Rothney, B.A., M.A., Ph.D.

Dean

of Arts

Masters

Ronald A. Anderchuk
Hon. B. A.

Honours

Hon.

B.

A.

(History)

(Economics)
Port Arthur, Ont.

Anton A. Brink

Bachelor of Arts
Gary

C.

Baldwin

Hon.

B.

A.

(English)
Fort Frances, Ont.

Port Arthur, Ont.

�151

�Donald
Hon.

E.

Thomas

Lake

F.

MacLeod

A.
(English)

Hon.

Fort William, Ont.

Port Arthur, Ont.

B.

B.

A.

(History)
&lt;2Sk

T*

"USE'

Jennie J. Masynyk
Hon. B. A.
(English)

Port Arthur, Ont.

John McClelland
Hon. B. A.
(Economics)

(Psychology)

Port Arthur, Ont.

Donald G.
Hon.

B.

Walter Petryshyn
Hon. B. A.
Fort William, Ont.

Mayhew

Bernard T. V. Skula
Hon. B. A.

A.

(History)

(History)

Fort Frances, Ont.

Fort William, Ont.

Bachelor of Arts
William H. Anderson
B. A. (Geography)
Winnipeg, Man.

Linda M. A. Angus
B. A. (Psychology)
Fort William, Ont.

Ronald A. Anderchuk
B.

A. (Economics)

Port Arthur, Ont.

152

�Victoria V. Archuk
B.A. (Englsih)

Timothy A. Aylward

Quibell, Ont.

Geraldton, Ont.

B.A. (History

&amp;

Political Science)

Clarence Battiston
B.A. (Economics)
Fort William, Ont.

Frederick N. Balina
B.A. (Sociology)
Fort William, Ont.

Baumann

Richard J. Battiston
B.A. (Economics)

Berthold

Fort William, Ont.

Fort William, Ont.

F.

B.A. (Geography)

Robert C. Blaine
B.A. (Economics)
Fort William, Ont.

Bryan D. Bjerring
B.A. (Economics)
Fort William, Ont.

Maurice

J.

Paul G. A. Bourret

Bourret

B.A. (Geography)
Port Arthur, Ont.

B.A. (Economics)
Port Arthur, Ont.

153

�Lawrence

J.

Bryan

Kathryn A. Buie
English)

B.A. (History

Fort William, Ont.

Fort William, Ont.

Chisamore

Jo-Anne Cain

Donald

B.A. (Sociology)

B.A. (History)

Eagle River, Ont.

Marathon, Ont.

C.

Donald Cordingly

Carol Coski

F.

&amp;

B.A. (English)

B.A. (English)

B.A. (Psychology)

Fort William, Ont.

Thornhill, Ont.

William

Greig Crockett

J.

Downey

B.A. (English)

B.A. (History)

Fort William, Ont.

Kenora, Ont.

Duhamel

William M. Ducasse

Ronald

B.A. (History)

B.A. (English)

Dryden, Ont.

Port Arthur, Ont.

154

J.

�i

Larry G. Earl
B.A. (English

&amp;

French)

Fort William, Ont.

Robert 0. Ekholm
B.A. (History)
Port Arthur, Ont.

Robert J. Elvin
B.A. (English)

Arnold Enders
B.A. (Psychology)
Geraldton, Ont.

Fort William, Ont.

Aid Suit.

Mary M. Evans
B.A. (Mathematics

&amp;

Karilyn K. Fedyk
B.A. (Psychology)

English)

Fort William, Ont.

Fort William, Ont.

Janine Feely

Philip Fiorip

B.A. (French)
Fort William, Ont.

B.A. (Philosophy)
Rort Arthur, Ont.

1
Mary

Nancy

C. Foley

P.

Fotheringham

B.A. (English)

B.A. (English)

Port Arthur, Ont.

Port Arthur, Ont.

155

�David

E.

Rhoda M. Gamble

Frederickson

B.A. (English)

B.A. (English)

Atikokan, Ont.

Dryden, Ont.

Foster W. C. Gauley
B.A. (Geography)

B.A. (Economics)

Fort William, Ont.

Fort William, Ont.

Robert C. Gerry

Arden

J. Gillis

B.A. (History)

Balmertown, Ont.

Thomas Goodman

David

B.A. (Political Science)

B.A. (English)

Fort William, Ont.

Brantford, Ont.

Alexander

B.

Gordon

C.

Goold

Fred

T.

M. Gray

B.A. (English)
Port Arthur, Ont.

B.A. (English)
Fort William, Ont.

156

��Dennis

E.

Johnson

B.A. (History)
Port Arthur, Ont.

Jean A. Jordan
B.A. (English)
Port Arthur, Ont.

Sandra G. Knight
B.A. (English)
Fort William, Ont.

George Kostyshyn
B.A. (History)
Fort William, Ont.

Maurice A. Ktytor
B.A. (Economics)
Fort William, Ont.

158

�Gary Kunnas

George Kurbatoff

B.A. (Economics &amp; Political Science)
Port Arthur, Ont.

B.A. (Psychology)
Fort William, Ont.

Kathleen M. Kuz
B.A.

Joyce Kyryluik

(German &amp; Psychology)

B.A. (Psychology)
Fort William, Ont.

Port Arthur, Ont.

Rene Larson

John Lee

B.A. (Political Science

&amp; Economics)

B.A. (History)

Marathon, Ont.

Port Arthur, Ont.

Herbert W. Lehtinen

Donald Lees
B.A. (Political Science

&amp;

B.A. (Economics)

History)

Port Arthur, Ont.

Fort William, Ont.

Antonio

Eileen E. Lehto
B.A. (French)
Port Arthur, Ont.

E.

Leroux

B.A. (English)
Fort William, Ont.

159

�Ian

S.

MacLeod

B.A. (English)

Sioux Lookout, Ont.

160

�Gregory A. Menuz

Cameron

B.A. (Economics)

D. Minor
B.A. (History)

Fort William, Ont.

Fort William, Ont.

Patricia

Donald
B.A

J.

L.

Kazumi Miyata

Mithrush

&amp;

B.A. (English)

B.A. (Psychology

Fort William, Ont.

Fort William, Ont.

Donald

Morrison

E.

Sociology)

Murphy

B.A. (French)
Port Arthur, Ont.

(Political Science)

Fort William, Ont.

B.A. (History)

William M. McLaren
B.A. (Geography)

Fort William, Ont.

Fort William, Ont.

Ruth

S.

McLaren

Velda McMillan

Ronald

B.A. (History)

B.A. (Psychology)

Kenora, Ont.

Kenora, Ont.

161

L.

Norris

�162

�163

�Lynne

C.

Erika Schmidt
B.A. (English)

B.A. (Economics)

Toronto, Ont.

Kenora, Ont.

Rod Shewchuk

Sihvonen

Ross B. Sinclair

B.A. (Psychology)

B.A. (History)
Port Arthur, Ont.

Fort William, Ont.

Emil

R.

Slivchak

B.A. (English)
Fort William, Ont.

Wilbur

R.

Donald M. Smith

Smalley

B.A. (History)

B.A. (Sociology)

Marathon, Ont.

Stouffville, Ont.

n
S
Lorna

E.

Bryan Springgay

Smith

B.A. (History

B.A. (Psychology)
Port Arthur, Ont.

&amp;

Political Science)

Port Arthur, Ont.

164

�Cynthia 0. Stadnyk
B.A. (French

&amp;

John

English)

R.

Stefiszyn

B.A. (Economics)

Fort William, Ont.

Fort William, Ont.

Edward Stewart

Richard A. Strey
B.A (Psychology)
Fort William, Ont.

B.A. (Mathematics)
Fort William, Ont.

Edith A. Strerz
B.A. (Psychology)
Fort William, Ont.

Gerald Swanson

M. Joan Stuart
B.A (English &amp; Psychology)

B.A. (Economics)
Atikokan, Ont.

Kenora, Ont.

Timpson

Gilbert Taylor

Paul

B.A. (Anthropology)

B.A. (English)

Port Arthur, Ont.

Wawa,
165

E.

Ont.

�Bernd H. Wedding
B.A. (German)

William G. Weiler

Port Arthur, Ont.

Fort William, Ont.

B.A. (Economics)

Bonita B. Wile

Julie Wierzbicki

B.A. (Psychology

&amp; Mathematics)

B.A. (Sociology)

Rouyn, Que.

Port Arthur, Ont.

166

�Faculty
of Science

John Hart, B.Sc, Ph.D.

Dean

of Science

Honours
Bachelor of Science

Frederick C. Briden
Hon. B.Sc.
(Mathematics)
Port Arthur, Ont.

Lome

John

B.

Hon.

B.Sc.

Evans

(Chemistry)
Fort William, Ont.

G. Everett

Hampe

Hon. B.Sc.

William W.
Hon. B.Sc.

(Biology)

(Physics)

Fort William, Ont.

Eagle River, Ont.

James

Hanneson

Hon. B.Sc.

Gerald M. Hashiguchi
Hon. B.Sc.

(Physics)

(Biology)

Port Arthur, Ont.

Fort William, Ont.

E.

167

�Bachelor of Science

168

�Thomas

G. Heritage

Gerald V. Hess

B.Sc. (Chemistry)

B.Sc. (Biology)

Port Arthur, Ont.

Port Arthur, Ont.

Peter

J.

Kantola

Donald G. Kerr
(Geology)

B.Sc. (Biology)

B.Sc.

Port Arthur, Ont.

Bowmanville, Ont.

Roman Kordiuk

Russell

(Mathematics)
Toronto, Ont.

B.Sc. (Chemistry)

B.Sc.

Kwiathowshi

Port Arthur, Ont.

Ann Lindstrom
(Mathematics)
Fort William, Ont.

Main

Betty

Glenn

B.Sc.

B.Sc. (Physics)

R.

Port Arthur, Ont.

Glenn A. Miller

Richard Middaugh
B.Sc. (Geology)
Simcoe, Ont.

B.Sc. (Physics)

Fort William, Ont.

169

�Charles N. Murphy
B.Sc. (Chemistry)
Port Arthur, Ont.

C.

Douglas McKessock
B.Sc.

Kennedy McLellan

Larry R. Peirce
B.Sc. (Chemistry)
Port Arthur, Ont.

B.Sc. (Chemistry)

Fort William, Ont.

John

Andrew

(Mathematics)

Port Arthur, Ont.

F.

James W. Redden

Penner

(Geology)

B.Sc. (Biology)

B.Sc.

Kenora, Ont.

Port Arthur, Ont.

Alasdair D. Smith

J. Sitarik

B.Sc. (Physics)

B.Sc. (Natural Science)

Port Arthur, Ont.

Fort William, Ont.

Harry

J.

Peter

Tsekouras

E.

Wynalda

B.Sc. (Physics)

B.Sc. (Physics)

Port Arthur, Ont.

Port Arthur, Ont.

17C

�Bachelor of Science

Sister

M. Josepha Walsh

in

Marlene

Nursing

P.

Yemchok

B.Sc. (Nursing)

B.Sc. (Nursing)

North Bay, Ont.

Fort William, Ont.

171

�University

Schools
H. S. Braun, CD., B.A., LL.D.
Director of University Schools

Forestry Technology

Donatd A. Buckley
Leshard, Ont.

Alexander J. Blakie
Inwood, Ont.

Guy

D. J. Depiero
Fort William, Ont.

Lloyd

Albert C. Hil
Devlin, Ont.

f

S.

Paul A. Malaguti
Welland, Ont.

W. Juhala

Port Arthur, Ont.

William Kinnear

Port Arthur, Ont.

172

Daniel

F.

Murphy

Ottawa, Ont.

�Donald

David R. Parsons
Willowdale, Ont.

E.

Patton

Port Arthur, Ont.

Sergio A. Perin
Fort Frances, Ont.

Roger Powell
London, Ont.

Gary A. Shea
Deseronto, Ont.

Ronald N. Simons

West

Hill,

Ont.

Ian F. Thompson
Toronto, Ont.

Auguste
Niagara

E.

Schmid

Falls,

Ont.

�Business Administration

Wayne

T.

Graeme

Aitken

Barr

Ottawa, Ont.

Port Arthur, Ont.

Donald A. Ferguson
Fort William, Ont.

174

�Olavi N. Pajunen
Nolalu, Ont.

Graham

Owen

R.

Michael A.

F.

Panula

Port Arthur, Ont.

Penny

Marja-Liisa Raty
Port Arthur, Ont.

Sound, Ont.

Stewart

Jeffrey B. Shivrattan

Clifford

Guyana, South America

Port Arthur, Ont.

Gary

L.

H. Shorrock

Port Arthur, Ont.

Edwin
Frederick T. Stirling
Port Arthur, Ont.

D.

J.

Yarzab

Fort William, Ont.

Frederick R. Wilmot
Port Arthur, Ont.

Robert W. Zachery
Fort William, Ont.

Murray Wilson

Port Arthur, Ont.

175

�Engineering Technology
1

Charles D. Bahrynowski
Brantford, Ont.

Brian S. Bida
Port Arthur, Ont.

W. Brown

Joseph W. Broczkowski

Leslie

Nipigon, Ont.

Port Arthur, Ont.

David

David

Dobbin

L.

C. Innes

Port Arthur, Ont.

Peterborough, Ont.
Robert G. Gallinger
Port Arthur, Ont.

Unto

T.

Frank S. Lappage
Dryden, Ont.

Kijanen

Port Arthur, Ont.

Lawrence

Oscar A. Mattas

Kakabeka

Falls,

T.

Mochizuki

Fort William, Ont.

Ont.

176

�Waldemar

John

A. Poluchowicz

B.

Sandmoen

Port Arthur, Ont.

Fort William, Ont.

Joseph O. Roy
St.

Catharines, Ont.

Roland A. Simard
Atikokan, Ont.

Em
E. Urquhart
Winnipeg, Man.

Lyle

Mining Technology

William Fotheringham

Gary Shields

Port Arthur, Ont.

Atikokan, Ont.

Clair D. Pilgrim

Allan A. Speed
Fort William, Ont.

Fort William, Ont.

Michael

J.

Whitton

Brockville, Ont.

177

�library Technology

Deborah A. Bryant

Iris

Fort William, Ont.

Fort William, Ont.

Barbara

E.

Davison

Conchie

Harry Deosaran

Fort William, Ont.

Trinidad,

Charlotte M. A. Elweit

West

Indies

Shirley A. Hall
Port Arthur, Ont.

Port Arthur, Ont.

Helen

S.

Fedor

Port Arthur, Ont.

Florence A. Harris
Fort William, Ont.

Carolee A. Park
Rainy River, Ont.

178

�Joan H. Perry

Zori L. Podbrscek
Port Arthur, Ont.

Murillo, Ont.

Deirdre M. Smythe
Port Arthur, Ont.

Research

Forest

Certificate
Paul A. Malaguti
Welland, Ont.

Daniel

F.

Murphy

Ottawa, Ont.

F.

John

R. Mihell
Sault Ste. Marie,

Brian

J.

Ont

Moore

Robert K. McCron
Port Arthur, Ont.

Woodstock, Ont.

Robert Nylund

David

Fort William, Ont.

B.

Roden

Kingston, Ont.

Auguste
Niagara

E.

Schmid

Falls,

Ont.

Gilbert W. Vanson
Oshawa, Ont.

179

�Gary Kunnas

Graduating

1

st

Vice-President

Class
Executive

1968

Joan Stuart
Secreta ry

Sharon Woods
Convener

Social

Chuck Grieve
Convener

Social

Debby Bryant

Mem ber-at- Large
Library Technology

Jean A. Jordan
Member-at-Large Arts

Fotheringham
Member-at-Large
Mining Technology
Bill

180

Thompson

Dave Dobbin
Member-at-Large

Ian

Engineering Tech.

Forestry Tech.

F.

Member-at-Large

�Jeff Shivrattan

Maurice Ktytor

Mem ber-at- Large

Mem ber-at- Large

Auguste Schmid
Member-at-Large

Business Admin.

Arts

Forest Research Tech.

181

Margaret Boone
Member-at-Large
Nursing Degree

�The always present and busy Bob Gude performs
duty

in

his

doling out portions of beef.

Beer and Beef

�To place graduating students in the proper mood
major events in their lives, the
Alumni Association threw a beer and beef party
for them and their guests. Hinds of beef and cases
of beer were plentiful and, most important, free
to all present. Eating, singing, dancing and drinking abounded as the grads let down their hair
as the climax of their university careers drew near.
for the forthcoming

�Convocation 1968

184

�Convocation 1968 was significant in that it was
the first time convocation ceremonies were held on
the campus of the university. Over 250 graduates
received their degrees and diplomas at the ceremony
in the C. J. Sanders' Athletic Building.
The

first

University

Master of Arts ever granted at Lakehead
received by Mrs. Diane Fawcett.

was

The guest speaker at convocation was Lord Caradon, G.CM.G., K.C.V.O., O.B.E., P.C., the Minister
of State for Foreign Affairs and Permanent United
Kingdom Representative at the United Nations.

set the theme for his talk on viothe world, since graduation exercises
paralleled the assassination and funeral of Senator
Robert Kennedy. He encouraged all the graduates
to develop a hatred of violence, to try and create a
better situation in the world.

Caradon

Lord

ence

in

After the ceremony, a reception was held in the
University Centre for all the graduates; parents and
friends.

185

�—

Convocation cont'd
Senator N.

AA.

Patterson

Chancellor.

(Above) R. Anderchuk, recipient of the
Governor General's Medal receives his
degree. (Above Right) The Chancellor presents

R.

Duhamel with

the

Chancellor's

Medal. (Right) The Master of Arts Degree,
Lakehead University's first, is conferred
upon Mrs. Diane Fawcett.

3

��Graduation

188

��190

��Awards
OR.

BRAUN'S MEDALS:
graduating students

for the highest ranking

in

University Schools.

Business Administration

Olavi N. Pajunen

Lawrence

T.

Mochizuki

_.

_

Engineering Technology

_

Forest Technology

Paul A. McAlister
Charlotte

M. Elwert

Library Technology

-

THE TREVOR PAGE MEMORIAL MEDAL:
for the highest ranking

William

graduating student

in

Mining Technology.

Fotheringham.

J.

THE SCIENCE MEDAL:
for the highest ranking

graduating student

in

the Faculty of Science.

part-time student

in

the Graduating Class of the

Frederick C. Briden.

THE CHANCELLOR'S MEDAL:
for the highest ranking

General or Honors Bachelor Degree.

Ronald

J.

Duhamel.

THE LIEUTENANT GOVERNOR'S MEDAL:
for the highest ranking

graduating student of the Third year of the General

Bachelor Degree.

Prudence

THE

F.

Morton.

GOVERNOR GENERAL'S MEDAL:
for the highest ranking student in the

lor

Graduating Class of the Honors Bache-

Degree.

Ronald A. Anderchuk.

THE PRESIDENT'S AWARDS:
Awards given annually
tions of responsibility

in

to the

who have

occupied posi-

and who by

their activities

graduating students

the students' organizations

and achievements have earned the gratitude

of the University.

William Weiler

A.M.S. President

Gerald V. Hess

A.M.S. President

Pentti Paularinne

Julie Wierzebecki

Bert

Arts Society President

and President

Bauman

Charles Grieve

Lome Gander
Raymond Halverson

of the

Graduating Class

A.M.S. Councillor and Winter Carnival Chairman
Chief Justice

Argus Editor
Nor'Wester Hockey Team Captain and S.A.S. Treasurer
_

S.A.S. Vice-President

THE POULIN AWARD:
An award for outstanding citizenship presented to the student selected by
fellows, the Faculty and Administration as contributing most to the welfare
the University through his student activities.

William Weiler.

192

his

of

�UNDERGRADUATES

�M. Abercrombie
Arts
I.

Aho

Arts
B.

1

Arts

1

Alexander
1

Anderson

B.Ad.

Ahokas

H.

Ry. En.
L.

D. Adam
Arts 1

1

S.

Sc.
R.

II

Alleyne

Adams

Arts
K. Aiajoki
Arts
I

I

T.

Amos

Arts

I

Anderson

Arts

E.

I

P.

I

Andros

Sc.

II

R.

Ahlstrand

En. Tc.
L.

Arts
K.

1

Albertini
I

Anderson

N. Deg.

II

R.

Aniuk

Arts

Arts

M. Armengaud

II

B. Ad.

I

B.Ad. Deg.
R. Asselin
B.Ad.
A. Au
B. Ad. Deg.
I

194

J.

I

Arthur

Apostolides

Sc.
P.

Ashby

Sc.

Arts

II

Avis
B.Ad.
I

B.

R.

J.

Arbouw

Arts

II

Arts

E.
I

S.

Arts
D. Asselstine
I

I

Science Building continues to
progress towards completion.

Anzew

A.

W. Andrusco

Atkinson

Ashlee

J.

I

0.

I

Atwood

Sc.

I

Ayers

B.Ad.

L.

Arts

II

G

I

II

Babcock

Arts

I

It

�Registration

Sept. '67.

M. Beagle

K.

Arts

Sc.

II

R. Bell

Arts
S.

G.

Babcock

En. Tc.
C.

Bailey

Com.
L.

Tc.

I

Ball

B.Ad.
II

Babichuk
I

L.

Arts

Baker

R.

En.Tc.

Sc.

I

Baranuik

Arts

L.

I

Barker

G. Barrette
B.Ad.
I

I

J.

II

II

M. Barkwell
Arts

II

G. Barron

B. Bartley

Sc.

B.Ad.

I

I

195

1

Bisby

Arts

Balabuck

B.Ad.

I

Lib.Tc.

I

B.

Arts

Backen

H. Bacchus
Sc.

G. Baillie
D.

II

Barone
%ts
H.

B.

Ry.Ar.

I

1

Bernauer

1

T.

Beck

F.

Sc.

1

Bellauance

Ry.En.

1

Berry
Arts
C. Bisenthal
Arts
J.

1

1

P.

Beda
II

B.

II

Beyak

Arts

Begay
1

Belmore

Arts

D.

Ap.Sc.
E. Benoit
Ap.Sc.
B. Birney
B.Ad.l

II

1

D. Blackburn

J.

Arts

Arts

1

Blackman
1

�J
J.

Blundon

B.Ad.
S.

Boyko

Arts

B.

Bodnar

Ap. Sc.
R. Bozynski
N.Deg. Ill
I

I

I

Boland

Arts II
P. Breitsprecher

O. Breton

R.

Com.

Com.Tc.

B.Ad.

Arts

Sc.

I

I

Construction on the
Residence Building
the spring thaw.

G.

Brown

Ry.En.

I

M. Burns
En.Tc.

I

G.

Brown

Arts

B.
Sc.

II

G. Burton
B.Ad.
I

^^^^^
it

Bollough

Bolitho
B.Ad. II
A. Braslins

L.

Arts
D. Bragnalo

B.

D.

Brunton

Busch
I

I

I

S. Botferill

K. Bottos

Arts

Sc.

I

I

I

Bottos
B.Ad.

L.

F.

Brickman

B.

Brodee

Sc.

II

Bone

Arts

I

I

D. Brooks

For.Deg.

II

I

new
began with

B.

Brymer

Arts

I

Arts

P.

f

II

P Buset
B.Ad.
I

Buckman

M. Bugara

J.

W. Buie

J.

Arts

Ry.En.
T. Butler

Arts II
H. Cameron

Arts

B.Ad.

B.Ad.

Arts

R.

I

Buset

Arts

I

Buie
I

II

I

R.

II

Cameron
II

L.

Bulmer

Arts II
V. Campigo
Sc.

I

�I

L.

Capricei

Ry.Ar.
T.

Chandler

Sc.

Caron

C.

Arts

I

S.

I

Carp

R.

Cheroski

Arts

Cheong

En.Tc.

I

Champagne

T.
J.

L.

II

Cheung

B.Ad.Deg.

I

A. Chan

C.

En.Tc.

Ap.Sc.

B.

Chu

B.Ad.

I

I

R.
I

Chan

C.

Chuchman

Sc.

Chan

Ap.Sc.

I

II

I

D.

Chan

B.Ad.

M. Chung

P.

Arts

En.Tc.

I

Chan

K.
Sc.

I

Chung

S.

I

Chung

Ap.Sc.

I

Additions to the University Centre
Building will vastly increase the
cafeteria facilities.

S.

Sc.

Ciglar

J.

Cole
Com.Tc.

Clark

Sc.

II

R.

L.

I

II

Collin

Arts

I

M. Clarke

B.

N.Deg.

Sc.

P.

Connor

Arts

II

K.

Clerihew
I

I

Conrad

Arts

B. Climie
Arts

II

w v

P.

Conroy

Arts

...

S.

Coghlan

Arts
A. Cooper
I

D.

Colborne

Arts

II

Cornell
Arts

J.

I

I

Jft

A. Cole

J.

En.Tc.

Arts

F.

I

I

C. Cotton

Cott

B. Ad.

Cole

II

Arts

II

I

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Arts

1

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1

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1

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1

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Lib.Tc.

D.

1

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Arts
1. Delorenzi

1

M. DiGiacomo
1

N.Deg.
B. Delgaty

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Arts

Arts

1

1

1

Devitf

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G. Drake
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1

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B.

1

B. Desilets

D. Doyle
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1

1

B. Currie

Arts

II

Depaola

Lib.Tc.

1

G. Cox

1

Davis

Arts

Arts

1

Douglas
N.Deg.
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Cummings

V. Dennisson

Arts

!

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II

Sc.l

Denis
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R. Dickson
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1

Danpier

P.

Covello

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Arts
D. Curtola
1

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1

Delorenzi
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N. Devraux
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1

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H. Drindak

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Arts

Arts

1

1

1

198

1

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Dunstan

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Esarek
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1

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1

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0. Fairbairn

Arts

1

1

Fold
Arts

T.

J.

J.

1

A. Fortier

Freeman

C.

Fallen

1

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M. Fredrickson

Sc.

Lib.Tc.

C. Gallucci

B.Ad.
A. Friske
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N.Deg.

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II

1

A. Fung
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L.

1

1

Gagnon

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1

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II

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D. Fry

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Forbes

J.

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1

Frankow

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1

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1

W. Fan
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Fotheringham

Arts II
J. Francis

P.

M. Ernewein
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1

J. Fallis

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1

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Arts

II

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1

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Sc.

1

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II

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Dziadyk

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II

D. Formica
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1.

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II

1

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J. Gaveil
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I

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Arts

V. Gay
Arts
H. Geddes
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V. Gay
Arts II
D. George
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II

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N.Deg.
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En.Tc.

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N.Deg. II
B. Gibson
B.Ad.

I

W. Golab
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I

Grann

II

200

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N.Deg.

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I

Graham
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J.

Goose

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D. Gouett

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N. Gorwill
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P.

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I

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I

Gougeon

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L.

Goose

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R. Goulet

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Arts

I

I

M. Graham

M. Graham

Arts

Arts

II

II

M. Gravelle

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Lib.Tc.

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Greene
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M. Greer

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Sc.

Arts
H. Grzelewski

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G. Gutsole

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Lib.Tc.

Arts
G. Hall
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Arts

A.
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II

Gruno
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Arts
J.

I

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Hamilton

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II

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Arts
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I

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I

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Arts

II

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Hamilton

Arts

I

G. Hansen
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A. Hanson

M. Hanzuk

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En.Tc.

I

J.

I

Hebditch

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Hickey
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J. Hindle

J.

Arts

201

II

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Hebert

R.

Arts II
B. Heikkila
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M.

L.

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Hill

Arts

II

J.

Hart

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G. Hilton
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R. Hiller

Arts

I

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1

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1

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1

Iwachewski
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D.

Holmstrom

Arts

1

J.

M. Hurdon

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Arts

Arts

Arts

II

Jackson
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1

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II

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Holmes

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1

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.

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photos taken here

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II

Jarrett

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II

1

G. Hucker
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II

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Arts

1

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R.

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Arts

1

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W. Hung

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G. Ironsides

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Arts

1

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D. Jennings

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1

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1

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Arts

II

J.

Johnson

Arts
G. Kobo
Eng. Tech.
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Arts

J.

1

U. Kijanen
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II

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Arts

1

L.
1

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R.

Sc.

1

C. Kelly

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1

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N.Deg. II
P. Kaszor

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J.

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C. Kartinen
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1

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1

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Sc.

II

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Arts

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Arts

1

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N.Deg.

Arts

to

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1

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M. Knaf

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1

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D. Kleinendorst

1

1

D. Kells

N.Deg.

1

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D.

W. Klages

West Indian

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Jordan

M. Kays
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1

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Arts II
G. Keffer

M. Kesmarky

Association
cast at

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1

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II

D. Kivilahti

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Sc.

II

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L.

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I

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I

Arts
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Sc.
S.

R.

I

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R.

Koen

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II

Kosowick

R.

I

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I

Kostas
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Arts

I

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T.

Sc.

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Krupay

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Arts

I

Kostrakewich G. Kostyshyn

Arts
R.

II

D. Krawchuk
Arts II

I

Kuppinen

En.Tc.

I

H.

Kurm

Arts II
A. Kwan
Sc.

II

C.
Sc.

Kuschak

J.

Kushnier

Arts

I

I

B.

M. Kwan

M. Kwan

R.

N.Deg.

Arts

Sc.

II

I

Kuzik

B. Ad.

I

Kwistkowski
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Lachman

M. Lachapelle

C.

Arts

W. Ladouceur

Labelle
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A. Lai

D. Laliberte

Arts
R. Lafrainere

Arts

Sc.

Arts

Arts

S.

Laban

N.Deg.
I

L.

II

II

II

I

I

�L.

Lage

Arts
J.

Lalonde

Arts
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D. Lahti
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I

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R. Lazar

I

I

Lambert

Arts

II

Lawrence

Arts

R.

I

D.
Sc.

I

Layman
II

G. Leatherdale
Arts
I

H. Laing
Arts II

N. Larsen
Sc.
F.

M. Laing
Arts
D. Latimer
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II

Law

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II

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Sc.

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Lee

J.

S.

I

I

W. Lee
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Sc.

B. Lehto

N.Deg.

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II

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Arts

L.

I

Lehto

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Lee
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M. Lee

M. Lechow

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Sc.
II

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I

I

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Sc.

I

Leggott

Arts

II

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Eng. Tec.

Li

Arts

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I

B.

Arts

D. Lichtman

S.

Arts

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1

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1

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1

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Arts

II

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Arts

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1

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Arts
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J.

1

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Arts

II

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Arts

1

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R.

II

McCailum

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1

1

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Arts

II

M. Mcintosh
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II

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MacAskill

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1

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R.

III

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MacDonald

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1

1

L.

1

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N.Deg.

1

MacMillan
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D. McCutchon

M. McBryan

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G. McGolrick
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J.

F.

1

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Arts

1

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Louko

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Arts

1

1

1

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Arts

1

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1

M. McDonagh
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Sc.

R.

McMillan

Arts

II

1

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1

1

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1

207

1

II

M. Melville
1

M. Metsaranta
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1

Minor

Arts

J.

McNicol

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1

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H. Matson

Arts

1

Merredew

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II

Miller
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II

Arts

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1

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D. Magnusson
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G. Maeba
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II

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II

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M. Muggaberg

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Arts

II

M. Morin

C.

Arts

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I

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Murray

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II

R.

Moore

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M. Nation

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I

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II

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1

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Muncaster
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MrowW

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G. Munro
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I

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R. Patterson
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Persaud
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Pallet

I

L.

Pentney

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I

Pappin

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R.

Paul

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I

T.

Paradis

I

J.

N.Deg.
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I

I

I

Perling

J. Pettit

I

Park

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Parker

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W. Pawluchuk

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Sc.

I

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I

Perlin

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Arts

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Perozzo

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N. Phillips
Arts II
I

210

I

G. Pearson
Arts
G. Perrier
Arts II
I

P.

P.

L.

I

Pehkonen

Arts

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Sc.

I

Parkins

B. Parrott

N.Deg.
D. Penner

Arts II
D. Pella

I

I

B.Adm.

Perry
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Perry
Arts III

R. Poirier

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J.
I

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T.

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A. Piatt

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C.

Putnam

Arts

II

R. Reid
Arts
R. Riddell
I

Arts

I

B. Potter

M. Powell

W. Presunka

P. Prior

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I. Rakovsky

Arts

Ry.Arch.

M. Rambali

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B. Rea

Arts

N. Quinn

Arts
G. Rajala

Arts

Sc.

Lib.Tec.

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Arts

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Eng. Tec.

I

I

U. Reinke
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M. Riekstins
Arts II
I

F.

Porter
I

M.

II

Reith

N.Deg.
L. Rintamaki
Sc.

I

II

J.

I

Rengert

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R.

II

Ramanciauskas
II

W. Repo
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I

M. Roach
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I

I

A. Richard
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I

M. Robin

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Sc.

Arts

I

I

Robinson
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Prystandski

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L

Reed

I

Reid

N.Deg.

I

II

D. Richard

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II

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-

I

Rodger
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Sc.

I

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I

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I

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Savitsky

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Saxberg

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Sc.

F.Deg.

I

Sc.

P.

Routhier

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Sanders

Arts

II

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P.

Ruddy
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I

I

Santoro

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II

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I

Sevean

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Sc.

I

I

Schnitzler

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I

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Sc.

Sc.

Arts

Arts

Sc.

II

Sarbadhikari

J.

J Scott

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I

C.

II

Arts

I

J.

I

Rudman

Arts
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M. Shahabudeen

I

B.

Arts

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I

Sheean
I

II

I

I

II

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F.

Sc.

Sc.

I

I

M. Rysinski

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Ry.Arch.
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Arts
M. Savatski

I

Sample
I

Lib.Tec.

I

M. Seabrook

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N.Deg.
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I

II

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II

II

if

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I

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II

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I

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II

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II

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Stewart

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II

I

D. Siddall

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J.

Sc.

L. Stirrett

Arts
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I

I

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I

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Sihvonen

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Sc.

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Sinnemaki

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D. Smith

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M. Talbot
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I

V. Trevisanutto
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I

L.

Strehlow

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I

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II

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Taylor

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Summers
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M. Tabor

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Tang

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Arts

R. Strickert

L.

S.

I

I

Thomas

I

W. Ticknor

J.

Ting

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Arts

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II

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Arts

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Arts

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I

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Arts

II

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Winters

Arts

II

Nancy Withers
N.Deg.
I

J.

Wright

Sc.
S.

Zaitzeff

Arts

I

M. Zee
Arts

I

M. Zuback
Arts

I

Yurchuk
N.Deg.

D. Yurick

L. Zanette
N.Deg. II

C. Zappitelli

J.

Arts

Arts

Zhgozewski
B.Adm.

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E.

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Sc.

E.

I

I

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I

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Lib.Tec.

I

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Eng. Tec
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I

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For.Deg.

R.

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Sc.

I

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I

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Arts

I

II

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I

216

I

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J.

Ry.Arch
A. Woischwil

Arts

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B.

II

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B.

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�217

�Jean Jordan
Assistant Editor

James

R.

Jed Drew

Zatulsky

Penny Connor
Undergraduates

Sports Editor

Editor-in-Chief

Just as the university

it

represents, Nor'Wester '68

had

its

growing pains

throughout the course of the year. But because of the dedication of a few
members of the staff they were overcome
We have increased our overall
.

From the

size in format,

number

The members of the

staff

which when

twice and then

Editor.

it

.

and we hope

quality.

who

countless hours of their free time
edition,

.

of pages, circulation

comes out

did come forward to work, gave up
and sometimes class time to put out this
will

probably be leafed through once or
But wait until that

placed on the shelf and forgotten.

shining black hair of yours starts turning grey. Then

when

you're looking

something on your book shelf you'll come across an old dust covered
edition of your Alma Mater's yearbook. Out of curiosity you dust it off and
open it. Immediately you forget about that greying hair and are drawn

for

218

�Nor'Wester Staff

Bill

Fred Wilmot
Sales

Edith Strerz
Sales

Gartrell

Graduates

Ralph Barone
Copywriter &amp;
Layouts

into your past, when both you and your unviersity were young. You'll recall
voyaging through vast oceans of mud to reach the classrooms, the Athletic
Building which never seemed to be completed on time, the wild Winter
Carnival, and the controversial Argus. For a while you'll be young again.

That

is

the purpose of a yearbook. Unlike

not a current events edition

Nor'Wester can do

worth

this for

—

it

is

a

its

brother a newspaper,

memory book.

If

this

it

is

edition of the

you, then the long hours of hard work will be

it.

James

R.

Zatulsky

Editor-in-Chief

Nor'Wester

219

Steve Gundry
Residence

'68.

Heather Laing
Faculty

�Acknowledgements
A yearbook
by time,

is

produced by the students for the students. However, being limited
and sometimes the technical knowhow, we, just like any

facilities

organization must rely upon assistance from other sources. Therefore,
like to

we would

express our sincere gratitude and thank those persons listed below, and

any others we may have inadvertently omitted, without whose assistance, the
production of our book would have been impossible.
Andrew's Photography

Photographs of the Frosh Queen
and princesses, Winter Carnival
Queen and princesses, Yearbook
Staff, club executives and the

Lome

Colour Photo of the University

inside liners.

Delinsky

crest

and many other valuable

photographs.
__..many valuable photographs,

Gerry Hashiguchi

especially the dedication page.

Tom MacLeod

Assistance with the

Chuck AAcOuat

technical information concerning

the University

title

pages.

and many valuable

photographs.

Graduate Photographs.
Cover design.

Pouncy's Studio
Stan Wojick

.

.

.

and also a very

special thanks to Jean Jordan, Jed

Directorate, for their unselfish giving of

of this

yearbook. Without

their

many

assistance

achieved.

220

Drew and

the Photo

long, hard hours in the production

our goal

could

never

have been

�����L1BRARY

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                    <text>����Nor 'Wester
Published

By The Students Of Lakehead University
Port Arthur, Ontario

Volume 20 Session 1968-69

Norma

R.

Ray— Editor

�Dedication

...

The Students Of
Lakehead University Dedicate
Nor'Wester '69

To
David Morgan

�Mr. D.W. Morgan

Mr. Morgan has spent the most recent years of his life in the Lakehead. He
received his B.A. from McGill University in 1948 and his M.B.A. from Harvard in 1950.
Before coming to Lakehead University, he was manager of the Ottawa store of Henry Morgan &amp; Co.
from 1951-'56 and manager of Dominion Securities Corporation from 1959-'62.

Born

in Montreal,

Mr. Morgan came to Lakehead College in 1960 and spent two years as a first year Economics
lecturer. In 1962, he became Bursar of Lakehead College. During Lakehead University's recently

Morgan has served in the capacity of Director of Finance from
1965- '67 and Director of Development from 1968- '69.
David Morgan is a man who is very much aware of community problems and seeks to be involved. At

successful development campaign, Mr.

Chairman of the Lakehead Board of Education, Chairman of the Board of Directors of
Army, and a Director in
the Mid-Canada Development Corridor Foundation.
In August, Mr. Morgan leaves Lakehead University to become an Economics Master of
Confederation College. It is with regret that we say farewell to a friend and wish him the best of luck
present, he

is

St. Joseph's General Hospital, Director of the Advisory Board of the Salvation

for the future.

3

�In

Our
University

Community

4

��6

�We

Enjoy...

Dances

7

���Message From

The Chancellor
Dr. William

J.

Cory, the famous Master of Eaton, once said:

"You go to a great school not so much
for knowledge as for arts and habits.

For the art of entering quickly into
another person's thoughts.

For the art of working out what is
possible in a given time.

For taste, for discrimination, for
mental courage and mental soberness."
I

sincerely

hope that you, who are leaving

this University, will

and habits" of which Dr. Cory speaks. In these days of violence,

have become familiar with the "arts
I

hope that you will have learned the

meaning of the expression "graduated terms" and "mental soberness" because such an understanding
will

be invaluable in the years ahead. Finally, we are proud of our University and

for

good wherever our graduates

go.

You,

with you, and the University's reputation

is

as graduates, will carry the

name

its

possible influence

of Lakehead University

dependent upon your future.

Senator N.M. Paterson
Chancellor,

Lakehead University

10

�Senator N.M. Paterson

11

�Dr.

12

W.G. Tamblyn

�Message From

The President
A yearbook, when looked at in the years hence, becomes a symbol of a definite period in your life a period in

which many attitudes were formed and many

vital decisions

were made. This particular

period has been one of almost unimaginable growth and change. There has been
within the university or within society generally.

And

yet

uncertainties within society itself that have contributed

I

believe that

it is

little stability

either

the ambiguities and the

more to the unrest among some students than

the conditions which they have found within their university community. In fact, the former

is

reflected in the latter.

It is

somewhat

immersed

most

ironic that the challenge

in an unprecedented

illusive.

demand

which faces today's graduate

for change at a time

when

is

one of orientation: he

a clear vision of the

is

"new order" is

While more familiar than his father with the possibilities of technology, he must employ

great creativity in forging the possible

and the practicable out of the potential which he has inherited.

Although the time that you have spent
both internally and externally,

I

hope that

at this university has

this has created in

capabilities so that

It is

social turmoil,

you an attitude of challenge rather than

one of despair. Whatever your future endeavours might be, you

and constructively.

been one of incessant

will

be called upon to think critically

our sincere hope that this university has assisted you in developing these

you are better prepared to meet the challenges that lie ahead.

We wish every success for the future.

Dr. W.G. Tamblyn,

President and Vice-Chancellor

Lakehead University

13

�Dean of Students
JohnW. Kerr
B.A., S.T.M. (McGill)

14

�Registrar of the University

Director of Extension and

Donald E. Ayre
B.A. (Sir George Williams)

Summer School

Kenneth L. Morrison
M.A. (Toronto)

Director of Admissions
WillD. Bohm
B.A. (Toronto)

Chief Librarian
Eric J. Belton
M.A. (Oxford)

Director of Planning and Physical Plant

Claude Smith
B.A.Sc. (Toronto) P. Eng., M.E., I.C.

15

�Administrative Officer
Physical Plant

Director of Northern Area Studies

Ted Broughton

C.D.,M.A. (Toronto)

Kenneth C. A. Dawson

Director of Athletics

George J. Birger
B.Sc, M.Ed. (South Dakota State University)

Director of Information Services
Charles D. McQuat

Director of Music
Boris Brott

16

�M.W. Bartley
M.S., Ph.D.

Chairman

Board Of Governors
Mr.

J.

Andrews

Mr. D.R. Lindsay

Machan

Dr. E. Arthur

Dr. J.R.

Mr. M.W. Babe

Mr. D.R. McMillan

Mr. L. Bode

Dr. D. Orr

Mr. C.J. Carter

Mr. J.N. Paterson

Mr. D.C. Clark
Mr. R.E. Costello

Rev. R.A. Peden
Mr. R. Philpot

Mr. G.P. Dalzell

Mr. R.J. Prettie

Mr. H.F. Dougall

Mayor E.H. Reed

Mr. J.E.J. Fahlgren

Mr. P. Ribotto

Mr. R.J. Flatt

Mr. B. Shaffer

Mr.

J.

M. Fleming

Dr. B.W. Stevens

Tuokko

Mr. E.L. Goodall

Mr. J.O.

Mr. T.S. Jones

W.G. Tamblyn
Mr. D.W. Morgan
Dr.

Mayor S. Laskin

17

�Faculty Of
Arts

18

�ARTS
PROFESSORS,
Mr. M.E. Arthur - History
Dr. F.M. Doan - Philosophy
Dr. C.L. French — Sociology
Dr. T.B. Miller - History
Dr. J.G. Rideout - English
Dr. A.L. Smith - English

ASSOCIATE PROFESSORS
Dr.

A.M. Akram — Psychology

Dr. A.A.D. Asismi
Dr. A.

—

Sociology

Chen — Sociology

Dr. K.M.

Dodd - History

Dr. E. Eager

— Political Science

Engholm — Political Science
Lewis — Modern Languages

Dr. G.F.

Mr. D.

- English
— Philosophy
Dr. P. Sarbadhikari — Political Science
Dr. J. Whittle - German
Dr. G.J. Merrill

Dr. W.S. Morris

ASSISTANT PROFESSORS
Dr.

Edward Bauman — Psychology

Miss Jeanne Bern — French
Mr. J. Cabot — Economics
Mr. Min-sun

Chen — History

Mr. D.F. Crozier — English
Mr. K.C.A. Dawson — Anthropology
Mr. M. Greenwood — Anthropology
Dr. J.F. Hilliker - History
Dr. F.M. Ishak - English
Dr. H. Loubat — Geology
Mr. S.R. MacGillivray - English
Dr. W.T.

Melnyk - Psychology

Mrs. A.M. Moscovitch
Dr. B.

- French

Mukhoti — Economics

- History
- Philosophy
Dr. K.P. Satinder - Psychology
Dr. A.A. Scholl - French
Mr. V.G. Wightman — Sociology
Dr. T. Yoon — Economics
Dr. E.R. Zimmermann — History
Dr. P. Raff o

Dr. R.C.S. Ripley

LECTURERS

Mr. A. Cloutier

— French

Mr. M.A. Colina - Spanish
Mr. I. Davies — Geography
Miss Marcia Dilley — Psychology
Dr. J.F. Evans

— Psychology

Mr. J.F. Futhey - English
Mr. B. Greenhous — History
Mr. E. Hughes - History
Mr. P.G. Johnson — Political Science
Mr. D. Kemp — Geography
Mr. A.O. Menhart - English
Mr. F.J. Nutch — Sociology
Mr. B.A.M. Phillips - Geography
Miss Vera Popov — Spanish
Mr. R. Shankman — English
Mr. R.W. Slocum — Economics
Mr. M.E. Smith - English
Mr. P. Wesley — Psychology

TEACHING ASSISTANTS

Miss Susan Abzinger — Latin
Mr. A. Alexander - Political Science
Mr. K. Allan - Psychology
Mrs. J. Alleyne — English
Mr. F.J. Anderson — Economics
Mr. L.M. Anderson — Psychology
Mr. D.M. Astwood — Economics
Mr. W. Bassil - Russian
Mr. J. A. Brigham - English
Miss Roseanne Candido — English
Mr. C. Charpentier — French
Mr. P.D. Chibos - Sociology

19

Mr. J. Braithwaite — Geography
Mr. B. Heggoe — Geography
Mr. A. Nabarra — Languages
Miss R. Tracy — Anthropology
Mr. P.G. Yurick - English

GRADUATE ASSISTANTS
Mr. E. Kolisnyk — Psychology
Mr. I. Kozyra — Psychology
Mr. R. Piovesana — History

�Faculty Of
Science

Dr.

J.

Hart

Dean of Science

20

�Dr. L. Hastings

SCIENCE

Dr. L.D.

Dr. D.G. Holah

PROFESSORS
Frood — Physics
Kent — Mathematics
E.L.P. Mercy — Geology

Dr. C.F.

Dr. S. Walker

—

- Chemistry

Hughes — Chemistry
Mr. E.J. M. Kendall - Physics
Dr. S.G.A. Magwood - Zoology
Dr. J.S. Mothersill - Geology
Dr. G.W. Ozburn - Zoology
Dr. D.W. Schwagerl — Mathematics
Dr. A.N.

Dr. D.G.

Dr.

— Physics

Hawton — Chemistry

Chemistry

Dr.

ASSOCIATE PROFESSORS

J.

Whitfield

— Mathematics

LECTURERS

W. Eames — Mathematics
Dr. W.M. Graham - Biology
Dr. J.S. Griffith - Mathematics
Dr. D. Orr — Chemistry
Dr.

Walter Bilyk - Mathematics
L.D. Black - Mathematics

Dr. V. V. Paranjape

Mr.
Mr.
Mr.
Mr.

ASSISTANT PROFESSORS

Mr. T. Norhtcott - Biology
Mr. D.W.A. Watson — Mathematics

W. Chu - Mathematics
L.D. Hansen — Mathematics
Mrs. M. Hawton — Physics
Mr. D.G. Hughes — Physics

— Physics
Dr. J.L. Talbot - Geology
Dr. J. Warren — Physics

Mr. W.R. Allaway - Mathematics
Dr. W.H. Baarschers — Chemistry
Dr. P. Barclay — Estrup - Biology
Dr. R. Freitag — Biology

GRADUATE ASSISTANTS
Mr. B.J. Cooke — Chemistry
Miss Pushpa Dua — Mathematics
Mr. D.A.H. Jackson - Physics
Mrs. S.B. Joshi — Physics

— Mathematics
- Science
Dr. G. Harvais — Biology
Mr. Eric Green

Dr. T.J. Griffith

21

�University

Schools

Dr. H.S. Braun

Dean of University

Mr. D. Alexander
Chairman: Business Administration

Mr. J.W. Haggerty
Chairman: Forestry

Mr. H. North
Chairman: Engineering

Mrs. C.J.W. White
Chairman: Nursing

22

�UNIVERSITY SCHOOLS

Mr.
Mr.
Mr.
Mr.

ASSOCIATE PROFESSORS
Mr. J. W. Haggerty — Forestry
Mr. W.J. Hanley — Business Administration
Mr. W.D. Mackinnon — Civil Engineering
Mr. H. North — Mechanical Engineering
Mrs. C.J. W. White — Nursing

M.N. Patterson
D.

— Mechanical Engineering

Roddy — Electrical Engineering

D.D. Sudar — Library Science
M. A. Zablocki — Business Administration

LECTURERS
Mr. A. Bartholomew — Forestry
Miss Margaret Boone — Nursing
Miss L. Butler — Nursing
Mrs. C.J. Faulkner — Nursing
Mrs. N. Kantola — Nursing
Mr. G.E. Phillips — Business Administration
Mr. J. Roberts — Civil Engineering
Mr. A.H. Seuret — Business Administration
Mr. J.R. Symington — Business Administration
Mrs. D. Syposz — Nursing
Dr. S. Zingel — Forestry

ASSISTANT PROFESSORS
Mr. D. Alexander — Business Administration
Sister M. Barbara — Nursing
Mr. M. Bjorgo — Library Science
Mr. W.R. Crowe — Business Administration
Mr. H.D. Elmslie — Business Administration
Mrs. L.E. Lyss — Nursing
Mr. G.R. Mott - Architecture

23

�LABORATORY TECHNICIANS

Mr. K. Pringnitz — Physics
Mr. W.P. Russell - Biology
Mrs. A. Sumpter — Geology
Mr. K. Sumpter — Instrument

Mr. George Angerson — Physics
Mrs. K. Andrews — Biology
Mr. R.L. Bennett - Geology
Mr. J.R. Butler — Instrument Room
Mr. J. A. Childs - Geology
Mr. D. Corbett — Chemistry
Mr. W.N. Currie - Audio- Visual Aids
Mr. D.C. DeKnock — Engineering
Mr. C. Fairbridge — Instrument Room
Mr. F. Foldy - Physics
Mr. J. F. Gateley — Chemistry
Mr. A. Harding — Chemistry
Mr. D. A. Jones — Chemistry
Mr. T. V. Jones - Chemistry
Mr. W.D. Lough — Instrument Room
Mr. W. A. Martens - Physics
Miss D. McLellan - Biology
Mr. W. Mettinen — Instrument Room
Mr. B.K. Morgan - Chemistry
Mr. J. Niemann — Geography

Mrs. M.

Room

Wahl - Geography

Mr. W.J. Wheeler — Engineering
Mr. R.L. Stephens — Seismograph

LABORATORY INSTRUCTORS
Mrs. M. Davies
Miss E. Vilcins

- Chemistry

LABORATORY ASSISTANTS
Miss C. Elwert - Library Technology
Mr. V. Gaudino — Languages
Mr. R. A. Schultz - Anthropology

24

�Memoriam

In

Thomas
On August

19, 1968,

Thomas

F.

Macleod

F.

MacLeod

('67) suffered a seizure

and died without regaining

consciousness.

Tom moved to

Fort William with his family in 1961 and he graduated from Fort William Collegiate
While at Lakehead University he was active in the Camera Club, the Yearbook, the Arts
Society Executive, and was Chief Proctor during the first two years of the proctor force's existence. He
was also a contributor to the Argus. Tom received his general B.A. in English and History in 1967, and
at the time of his death he was completing his Honours degree with the intention of continuing for his
Masters degree.
,

Institute.

The yearbook
loss of a valued

staff joins the rest of the University

community and

his family in

remembering the

member and a good friend.

'

;
.

'

'"'/&gt;'.•

•

�Alma Mater
Society

Peter

McCormack

A.M.S. President

President's Message
Being President of the A.M.S. is a challenge if one accepts the challenge. I often wondered over the year if I really had
so. The temper of the Council activity reflected my management of Council affairs, and it consisted of intermittent
sallies of politicization and social awareness countered by significant periods of indecision and the inevitable but often

done

necessary process of self-examination and analysis.

Council suffered somewhat from the feeling that progression must be the indicator of the value of an action. This is
not generally so, for circumstances and events may be intrinsically good. A universal standard will not do for the
measurement of the validity of human action until the universal standard is agreed upon by all. Needless to say, such

agreement is a lot to ask of twenty-five university students, and certainly there was no evidence of it last year.
I view my last year in A.M.S. with a certain degree of amazement. I was fiercely determined in my job. In light of this,
it is a wonder to me that I could have made as many mistakes as I did, and at the same time, it is distressing to think that
some of the mistakes made were of a purely academic nature. If one can perform well academically in university student
government, then that is at least good enough. The question of university in society is one of much broader scope, and
one which I am not prepared yet to resolve personally.
If these remarks seem somewhat pessimistic, it is only because I feel the weight, even now, of the responsibility
involved in a student government office. One cannot jump into the fore unconvinced about his position; if he does, then
he will be buffeted about by those who are heading in a definite direction. While I was and am certain of my ideas, I think
perhaps I failed to elucidate them well. This does not make me a failure; however, it stands as a drawback which I shall
continue to regret for some time, and from which I hope my successors will remain freed.
Peter

McCormack

June 1969

26

�Kax Miyata -

Vice-President of Programming
Dennis Wallace - Director of Finance

Peter McCormack

- President

Robert Gibson - Vice-President of Academics

FRONT ROW,

Left to Right: Bruce Brymer, Fred Poulter, Dennis Wallace, Peter McCormack, Pat O'Brien, John Hickey,

Miyata.

MIDDLE ROW: Mike Gravelle, Ken Boschkoff.
BACK ROW: Paul Paularinne, Dave Montgomery, Ed Otte, George Logan, John McCutcheon, Mike Pawlowski, Karen Moore.

27

Bob Gibson, Kaz

�Arts Society
President: Pat O'Brien

Vice-President: Paul Paularinne

Secretary:

Penny Connor

Treasurer: Khalid Ali

Science Society
President: Fred Poulter

Vice-President:

Don Asselstine

Dryan Probizanski
Treasurer: Dave Layman

Secretary:

University Schools
Society
John Hickey
Tom Fry
Secretary: Angela Hockley
Treasurer: Mike Pawlowski
President:

Vice-President:

28

��Larry Hebert

Second Vice-President

Ralph Barone
First Vice-President

Heather Laing
Secretary

Joan Danielson

John Sihvonen
Memher-At-Large

Member -at-Large

Arts

Arts
30

�Bill

Hodgson

Social Convener

Seppo Viherjoki
Member-at-Large
Business Administration

Frank Mitchell
Member-at-Large
Graduate Business Administra tion
31

Mary Nation
Member-at-Large
Library Technology

�Faculty Of Arts

Stephen Belle
Psychology

Eugene Kolisnyk
Psychology

32

�Honours
Bachelor Of Arts

Judith Calonego
English

33

�Barry Lyons

Psychology

34

�Pentti Paularinne

Geography

35

�Sara Weber
English

36

�Bachelor Of Arts

�38

�39

�40

�Anthony Dandridge
History

41

�Joyce Farrel
English

42

�M.E. Paullie Fredrickson
English

43

�Johann Goertz
Geography &amp; Economics

44

�45

�John Howard
Psychology &amp; Philosophy

46

�Elizabeth Irving
English

&amp; Psychology

47

�48

�John Lalonde
Economics

49

�50

�William Joseph Malinosky
English

51

�Louella Melynchuk

Psychology

52

�Lee Morrison
Sociology

Patricia

53

�54

�55

�56

�57

�David Siciliano

58

�59

�60

�61

�Honours Science

Geraldine Sandra Service

Mathematics

62

�General
Bachelor Of Science

Leonard Andrew Chaykowski
General Science

63

�Cheryl Ann Graham
Chemistry

64

�65

�Charmaine Anne Mazurkewich
Biology

Daryl

J.

McLellan

Biology

Brian A. Milanese

Mathematics

Eldon John Oja
Physics

66

�James William Redden
Geology
Frederick Harold Poulter

Biology

Owen Charles Trist
Mathematics

67

�Bachelor Of Science

Nursing

Sheila Jane

Coxon

�Kenneth Donald George MacDonald

69

�Walter Michael Wojcik

70

�Forestry

Technology

71

�72

�Business Administration

�74

�Frederick R.J. Wilmot

75

�Engineering

�Mining

Garry Wayne Shields

Allan Arthur Speed

BHHHHH^^HHHHIHMBHMHflH

Technology

Lloyd Heatley Chandler

Forest Research

Guy David Joseph Depiero

Albert Charles Hill

Gary Alan Shea

Ronald Norman Simons

David Robert Parsons

77

�78

�Lorna Lenore Hill

79

�Margaret Joan Voloshin

80

��I

have extremely enjoyed this past year as President of the Lakehead University Student Athletic Society.

I

feel

our

programme has proceeded fairly well as was evidenced in the immense growth in our spectator sports and general over-all
increase of school spirit. This is very important as nothing is better or more conducive to having a sound University
image across the country than a sound athletic programme and this has been displayed through our resounding success in
most athletic contests this year.
In the major inter-collegiate sports such as hockey and basketball, we had very good seasons with an extremely active
turnout by all students. This trend, hopefully, will continue, and I am sure it will, along with the calibre of the sports
involved.

At

this

time

last

year

I

stated that

we would

strive

even harder to improve athletics especially in the Ontario
we won four championships while placing second,

Inter-Collegiate Athletic Association championships. This year

fourth, and fifth in others. It was rather interesting that in the skiing championship where we finished second, we were
beaten by a team of Lakehead graduates now attending law school at Osgoode Hall. We also competed for some
Canadian championships in sailing and swimming and here we placed almost as well while maintaining Lakehead
University's athletic image.

The

and Council along with the Athletic Department were tremendous this year and there was a
and help from all people involved. This is where the year was most successful, and why the
student has been able to participate as fully as he or she did. Next year's executive looks very good, and along with the
addition of the S.A.S. Assistant Intramural Director, should continue to promote athletics to an even higher level.
In concluding I would like to thank everyone who participated and competed in our athletic programme, therby
enabling me to have a wonderful and successful year, as well as making athletics so successful for Lakehead University.
S.A.S. Executive

great deal of co-operation

Bruce Brymer,
S.A.S. President

82

�S.

A.S.

Executive
Bill Hepditch - Treasurer
Bruce Brymer - President
Gord Skinner - Vice-President
Maureen Broadhurst - Secretary

S« A* S.

Council
FIRST ROW,

Left to Right: B. Brymer, V. Vanier, G. Skinner.
T. Timmons, M. Riekstins, M. Broadhurst, B.
Hepditch, C. Montgomery, L. Hebert.
THIRD ROW: B. Tees, T. Fry, D. Holmstrom, J. Pallett, J.

SECOND ROW:

Kennedy.

ABSENT: D. Vickruck, R. Hiller, D. Goodwin, G. Walford, J.
Johnston, A. Holt, R. Cameron, L. Pero, N. Dahl, A. Chan, M.
Urquhart, D. Oldham, B. Dubois, Z. Machelak.

83

�84

�Awards
MALE ATHLETE OF THE YEAR: Murray Smith
FEMALE ATHLETE OF THE YEAR: Glenis Holmes
HONOUR ATHLETES: Dave Siciliano

Golf:

Dave Kerr
Grant Forbes

Murray Smith

Albert Swieca

Don Holmstrom
Lou Pero
Rob Cameron

Dennis Halabecki
Table Tennis:

Larry Hebert

Stephen Belle

Bruce Brymer

Anthony Lai
Kevin Lau
Wai Poon

Marita Riekstins

Maureen Broadhurst
Judy Perlin

Skiing:

VARSITY LETTERMEN:
FIRST YEAR:

Dan Hennefent

Cardigans

SECOND YEAR:

Hockey:

Jackets

Gordon Bishop

Don Gutsole

Hockey:
Dwight

Ray Hunt

Stirrett

Bruce Nelson
Rick Peotto
Dave Rennie

Richard Tapak

Vern Campigotto

Jim Pronger

Bill

Dave Nuttall
Denis Laliberte

Webb

Peter Lenardon

Basketball:

Gordon Walford
Basketball:

Wayne Humphreys
Dan Carroll
Phil

THIRD YEAR:

Plaque

Fury

Willie Jerks

Hockey:
Dave Siciliano
Murray Smith

Richard Earl

Dennis Portman
Fencing:

Basketball:

John McLeod
Clinton Kushak
Bob Ayres

Lou Pero
Don Holmstrom

FOURTH YEAR:

Blanket

Curling:
Basketball:

Rick Moats

Rob Cameron

Peter Jensen

Tom
Cal

Fry

Montgomery

Golf:
Bill

85

Hodgson

�FRONT ROW: B.Nelson, D. Nuttall, R. Tapak, D. Gutsole, D. Siciliano, M. Smith, H. Matson.
BACK ROW: D. Young, Trainer; J. Kennedy, D. Stirrett, J. Pronger, R. Hunt, R. Peotto, M. Tracey,

D. Rennie, V. Campigotto, H. Akervall,

Coach; P. Lenardon, Manager.

ABSENT:

J.

Gellert, D. Laliberte, D. Ostaff, B.

Webb,

C. Tuyl, G. Bishop,

J.

Snopek, E. Moores.

Inter- Collegiate

Hockey

The Lakehead University Nor'Wester Hockey team placed third in the
Hockey Association with 8 wins and 8 losses.

International Collegiate

Named

to the I.C.H.A. All-Conference

team were Dave

Siciliano,

Murray

Smith, Dwight Stirrett and Gord Bishop. Dave Siciliano and Murray Smith

were also named to the National Association of Inter-Collegiate Athletics
All-American Team.

86

�FRONT ROW: R. Panfil, M. Siemieniuk, R. Cameron, W. Humphreys, R. Earl, M. Davis, L. Hebert.
BACK ROW: J. Brownrigg, Assistant Coach; G. Birger, Coach, L. Koski, D. Holmstrom, W. Jerks, P. Fury, D. Carroll, A. Haapaiemi, L. Pero, G.
Walford, Manager.
MISSING: R. Woods, D. Portman.

Inter- Collegiate Basketball
The Nor'Wester Basketball team had

a

good season

record of 18 wins and 9 losses. High scorer was

433 points
direction

in

this

year with a

Wayne Humphreys with

27 games. This team has great potential under the able
Birger and can look forward to winning the

of Coach

championship next year.

87

�O.I.A.A. CHAMPIONS
Dave Kerr, Dennis Halabeck, Grant Forbes, Albert Swiecca,

Bill

Hodgson,

Bill

Shannon, Coach.

Inter- Collegiate Golf
The O.I.A.A. Golf Championship was hosted by Trent University

last

fall in Peterborough. With eight teams participating, the Lakehead Team
placed first with 631 points, Osgoode Hall was second with 646 points
and Waterloo Lutheran placed third with 647 points.

88

�O.I.A.A. CHAMPIONS
Rick Moats, Skip Peter Jensen, Third;
;

Tom Fry, Second; Cal Montgomery, Lead.

Inter- Collegiate Curling
For the

first

time Lakehead University was host to the Ontario

two days of
Lakehead team, skipped by Rick Moats, defeated Osgoode
Hall, Waterloo Lutheran and Trent to win the O.I.A.A. Curling
Championship with a perfect 5-0 record. Ryerson defeated Brock, York
and Laurentian to win the Consolation.
Inter-Collegiate Athletic Association Curling Bonspiel. After

curling, the

89

�Glen

Miller,

George Ozborne, Coach; John

Fallis,

Tom

Petrie.

MISSING John Sihvonen, Allan Holt.
:

Inter- Collegiate Squash
The O.I.A.A. Squash Tournament was hosted by York University this
Championship team earned 17 points while Osgoode
Hall was a close second with 15 points. Lakehead placed fifth in the
year. Ryerson, the

tournament.

90

�FRONT ROW: G. Cancade, D. Hennefant.
BACK ROW: B. Shannon, Coach; C. Doyle, D. Speed, T. Burke, B. Friday.

Inter- Collegiate Skiing
Lakehead University was well-represented in the O.I.A.A. Ski
Championship held at Laurentian University. They placed second to
Osgoode Hall with many of the top Osgoode team members being
ex-Lakehead University students.

91

�Inter- Collegiate

Swimming

Lakehead University, for the first time, entered the O.I.A.A. Swim
meet with the smallest team entered. Although we only placed fifth, Dave
Curtis was chosen to represent Lakehead in the Canadian Inter-Collegiate
National Championship at the University of New Brunswick.

92

�FRONT ROW: M.C. Zuback, J.A. Pettit.
BACK ROW: L. Tracey, C. Hagstrom, D. McDonald, L. Logozzo, L. Adams, L. Bonnett

Cheerleading
The Lakehead University Cheerleaders had a busy year during
1968-1969. They devoted a great deal of time and effort to help promote
school spirit and are to be congratulated on a job well-done.

93

�FRONT ROW: Gail Amort, Jackie Turner, Helen Morrish.
BACK ROW: Jackie Hoffman, Wilma Van Den Hurk, Linda Thomas, Judy Perlin, Glennis Holmes, Marita Riekstins, Bill Shannon, Coach.
ABSENT: Linda Hornblower.

Women's Basketball
The Lakehead University Women's Basketball team had a good season
under the direction of their coach, Mr. Bill Shannon. At the end of the
season their record stood at 12 wins and 4 losses and they were the
Champions of the Thunder Bay Basketball Association Senior Women's
League. The top scorers were Glenis Holmes with 172 points and Judy
Perlin with

156 points.

94

�FRONT ROW: Molly Mclntyre, Donna McDonald, Debbie Haggerman, Sandra Chepil.
BACK ROW: Kathy Kangas, Coach; Barb Madwick, Barb Caldwell, Barb Kozub, Celina Reitberger.
ABSENT: Ann Gordon, Barb Jackowski.

Women's
The Lakehead

University

Volleyball

Women's Volleyball Team,

in it's first year,

4 wins and 4 losses. They also
received the runner-up trophy at the Hibbing Invitational Tournament.
The most valuable player on the team was Barbara Medwick.
had a

fairly

good season with

a record of

9b

�Inter- Collegiate Fencing
Competing against three other teams, the Lakehead University Fencing Team placed first in the O.I.A.A.
Fencing Tournament held at Brock University. Second place was York University and third place was Brock.

Inter- Collegiate Table Tennis
The O.I.A.A. Table Tennis Tournament hosted by Osgoode Hall saw the Lakehead
team defeat seven other teams to place first with a record of nineteen wins and two
losses. Second and third places went to Brock University and Ryerson respectively.

96

�97

�93

��Argus Staff

SQUATTING, Left to Right: John McGregor, Bob Leggett, Al Roblin, Simon Hoad.

AT TABLE,

Left to Right: Barb Williams,

STANDING,

Wendy Wilson, Ron Baker, Marnie Stewart, Linda Montgomery.

Left to Right: Gord Ackri, Winston Rennie,

Doug Smart, Gord Fukushima, Doug Angus, Clayte Petrick.

100

�c.u.s.o.
LEFT TO RIGHT: Jeanetty Gall, Student Chairman; Sharon Inouye,
returned C.U.S.O. volunteer; Andre Cloutier, Faculty Representative

Business Club
Dennis Buset, President; Jim Blundon, Vice-President; Glen Burton, Treasurer (ab.) Les
Tippin, Secretary (ab.).
;

Chinese Student Association
David Lee, President; Steve Wong, Vice-President;WaiHonPoon, Treasurer; DavidHui,
Secretary.

101

�Circle

K

Mike Pawlowski, President; Paul Sebesta, Vice-President; Seppo Viherjoki, Secretary
Treasurer; Jerry Bums, Director (ab.)

Drama Club
Ian Maplethorp, President; Elvene Hamilton, Secretary Treasurer.

Engineering
Institute

Of Canada

Dave Lawrence, Chairman; Emilio Righto, Secretary Treasurer;

Norman Horofke, Vice-Chairman.

102

�)

Engineering Society
Dave Molson, President; Mike Kohanski, Secretary Treasurer; Andy
Saj, Vice-President.

French Club
Bruno

Desilets,

President;

Michael

Metherell,

Vice-President; Rita Hunt, Treasurer; Lita Boubreau,

Secretary;

Mark Boubreau,

Advertising; Marcia Hardy,

Social Convener; Wendi Ficek, Social Convener.

Judicial

Committee

Ralph Barone, Associate Justice; Doug Loken, Associate Justice; Bill
Cocker, Court Clerk; Mike Barkwell, Chief Justice (ab.);Tony Hill, Crown
Attorney ( ab. ) Bob Murray, Defence Attorney ( ab.
;

103

�L.U.F.A.
John North, President; Steve Gundry, Co-Ordinator; Bob Yatkowsky, Assistant
Public Relations (ab.); Shawn Cooke, Public Relations; Rich Clarke, Secretary;
Herb Bax, Treasurer; Ross Singleton, Vice-President (ab.)

L.U.N. A.
Sharon Weller, President; Leslie Reid, Corresponding Secretary;
Janet Perling, Recording Secretary.

Anne

Piatt, Treasurer;

L.U.S.T.
Ian Maplethorp, Producer; Val Dennison, Assistant Producer (ab.)

104

�Political Science

Club
Doug Loken,

President; Beth

MacKinnon, Publicity Chairman; Michael Metherell,

Vice-President.

Sociology— Anthropology Club
Angela Winchester, President; Sue Erwin, Vice-President; Ted Christiansen, Treasurer;
Jim Doherty, Recording Secretary (ab.)

105

�West Indian Club
Angela Winchester, President; Mike Rambali, Vice-President; Roger Shim, Public Relations Officer; Chunirai Lachman,
Treasurer; Lois Fredricks, Secretary.

Winter Carnival
Russ Percy — Chairman
Marcia Graham — Co-Director
Les Tippin — Treasurer
Bob Katajamaki — Co-Director
Sandra Borton
JudieGraveson
Susan Friday
Beth MacKinnon

Sharon Weller
Ekins
Pat Gain
Joanne Burak
Karen Moore
Bill

BayneByak (ab.)
John North (ab.)

Ray Walker (ab.)
Mike Sweeney

Steve Gundry
Darlene Cumbalisty

(ab.)

AlanRoblin(ab.)
106

��In Residence We...

�Create

109

�WELL

.

.

.

WHILE THE OTHERS

SOME DO

110

.

.

.

���Frosh

Sept. 16:

Week

Science Assembly

Arts Luncheon

Student-Faculty Reception
Sept. 17:

Business Administration Dinner

Arts Faculty Movie
Roller Skating

Sept. 18:

Films
S.D.U. Presentation

Sept. 19:

Films

Chippewa Park - Science
Centennial Park
Sept. 20:

-

Arts

A.M.S. Dance

Sept. 23-26: Science Receptions

Sept. 27:

A.M.S. Elections
Arts Society Dance

�114

�United Appeal

Comes

To
Lake head
University

Via

The
Engineers

115

�October...

116

�117

�118

�119

�120

�121

�November..

�The Manitoba
Contemporary
Dancers

123

�In Concert

124

�S. A.S.

Homecoming

125

�December...

�New
Years

Eve

��January...

Winter

Carnival
'69

�130

�King Karnival:
Dennis Wallace

The King's
Duty??

131

First

��V

''''^VHHHHHH

Winter
Carnival

Parade

Engineering

Business Administration

And Nursing Degree
133

��Mark Twain
At

Home

��137

��lptures

69

Days

�140

�141

�142

�143

���Did You Say Play Money???

�Car Bash

The

Good Fortune
147

��149

��151

�152

�1

i

King:

Queen:

Dennis

Donna

Wallace

Pace

—Business

—Arts
Administration

153

�Carnival Queen

Donna Pace
Faculty Of Arts

�Miss Business

&amp;
Nursing Degree

Connie Reid

Miss Engineering
Liz

Adams

155

�Miss Science

Lynn Hauta

Miss Nursing

Marie Ferguson

�Miss Forestry
Diane Nylund

Miss Library Tech

&amp;
Ryerson Arch.
Gloria Balon

157

�158

�159

�160

�Pozo-

Seco

161

��163

��165

�S. A.S.

�O.LA.A. Curling
Champions

Bruce Brymer
President, S.A.S.

Glennis Holmes

Female Athlete

Of The Year

Murray Smith
Male Athlete

Of The Year

��April...

���Alumni

172

�173

�Convocation

1969

Degrees and diplomas were presented to 387 graduating students Saturday, May 31 at Lakehead University's
Convocation Exercises.
A total of 217 students graduated from the Faculty of Arts including Lawrence Hansen, a mathematics major who
received the University's second Master of Arts Degree. General Bachelor of Arts degrees were presented to 190 students
and 26 Honours B.A. degrees were awarded.

The Faculty of Science graduated 49 students this year including nine Honours B.Sc. graduates.
Degrees and Diplomas were awarded to 121 students from the University Schools. This total included 32 from the
Bachelor of Science in Nursing program, six graduate diplomas in Business Administration, nine from Forest Research,
one from Mining and 20 from Library Technology.

The executive Vice-Chairman of

the

Committee of Presidents of

guest speaker at the Convocation exercises.

174

Universities of Ontario, Dr. J.B.

Macdonald was

�Awards
Winners

POULIN

AWARD

:

for outstanding citizenship presented to the student

selected

by

Faculty and Adminimost to the welfare of the

his fellows, the

stration as contributing

University through his student activities.
Pentti Paularinne

PRESIDENT'S AWARDS:

given annually to the graduating students who
have occupied positions of responsibility in

who by their
and achievements have earned the

the students' organizations and
activities

gratitude of the University.

Don Bergman
Maureen Broadhurst

Peter

McCormack

Jeanetty Gall

John McCutcheon
Glenn Miller

Larry Hebert

Pentti Paularinne

Don Lees
Owen Marks

Mary Powell
John Sihvonen

Wendy Ticknor
Dr. Braun's

John C. McCutcheon

Medal
for the highest ranking graduating student in Business Administration

Dr. Braun's

George Barrie Reed

Medal
for the highest ranking graduating student in Engineering

Dr. Braun's

Medal

Herb Arnold Bax

for the highest ranking graduating student in Forest
Dr. Braun's

Technology

Technology

Nancy Doreen Marks

Medal
for the highest ranking graduating student in Library Technology

The Science Medal

Douglas John Robert McKessock, B.Sc.

for the highest ranking graduating student in the Faculty of Science

The Chancellor's Medal

Eleanor Joan Miller, B.A.

for the highest ranking graduating student in the Graduating Class of the General or

The Lieutenant Governor's Medal

Honours Degree

Colleen Sheila Mahoney, B.A.

for the highest ranking graduating student of the Third year of the General Degree

The Governor General's Medal

Owen Marks,

for the highest ranking student in the Graduating Class of the

175

Honours Degree

B.A.

�The Opening

176

of the Ball

�177

�Of H6e fyaduatUy (fym,
/tact rf(C

Of

*%efi

Executive

'pot TKatiwcf, Oocx tyiadua£i&lt;M

One

TRemem&amp;e*.

�Doing Our

Thing

179

Own

�180

�181

�182

�133

�184

��Nor'Wester
Staff

Nor'Wester 1969 got off to a slow
first

had trouble in finding a person with few enough
some of the activities that you remember from the beginning of

start this year as last year's staff

brains to take the job as Editor-in-Chief. For this reason

term have not been represented.

To some, a yearbook is just another piece of junk to be stored away and forgotten but to a few of us, it will bring back
many happy memories of our years at Lakehead University.
We, on the staff, realize that this may not be the best but we tried to make it worthwhile. Without the help of the
photographers, Don Bergman and David Lawrence and the copywriters and layout artists, Maureen Broadhurst and Gail
Keffer this year's Nor'Wester would never have existed. To all the others who gave up even one evening of their time in
order that Nor'Wester '69 could be published, we thank you.

186

�Acknowledgements

The

staff of

Nor'Wester '69 being fairly small, we were
many people for assistance. We would like

forced to rely on

to express our sincere gratitude to those listed below and to

any that we have inadvertently omitted.

Gord Acri

Sports Title page

Andrew's Photography

Photographs of the
Winter Carnival Queen
and princesses.
Photographs of the

Tony

Allard

University buildings.

L.U. Information Office

Copy

Pouncy's Studio

photographs
Graduate photographs

material and

several

187

�We

Tried

188

����I

�INTER -COL LEG ATE PRESS OF
I

CANADA

1315 Inkster Boulevard, Winnipeg
Publishers

14,

- Manufacturers

Yearbooks — Yearbook Covers
Graduation Announcements
Diplomas

LTD.

Manitoba

��1

k

[

i

-

1

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                    <text>��LAKEHEAD
UNIVERSITY

GEOLOG Y

JOURNAL
1st

EDITION
1970-71

EDITOR
JURIS ZDANOVSKIS

CO-EDITOR
PATRICK FUNG

�.

All the woric you've
done in the past few
years is about to pay off

Our congratulations.
You’ve worked hard to get
And we’d like to see you

African Selection Trust. With

world-wide interests in gold,
copper, diamonds, molybdenum

this far.

get a lot further.

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With

And

us.

we’re

and other minerals.
So when something good
comes along, we’re not afraid to

in-

volved in exploration activities

Canada and

the United States.
use the most sophisticated techniques in the fields of
geology, geochemistry and geophysics. Because that’s just the
way we think a job should be
in

We

finance it. And your talent just
could be one of those good things.
Even if you’re not graduating
this year, you could join us for the
summer. Then when graduation
comes, you’ll be ready.
So think about your future
with us.
After all, you’ve earned it.

done.

So when you work with us,
you work with the best. And you
also have the best support behind you.
Selco is backed by the combined assets of England’s Selection Trust and by Consolidated

Selco
6th

2

floor,

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�*Detlica£i&lt;M
It is appropriate that this first
volume of the yearbook be dedicated to
Dr. Edward Mercy.
Dr. Mercy came to
Lakehead University in 1967 to set up
the Department of Geology and so this
year marks the first year in which the
graduating honours students will have
received all of their university training under Dr. Mercy’s excellent guidance.
Dr. Mercy came to Lakehead
University after a distinguished ten
year career at the Grant Institute of
Geology at the University of Edinburgh.
He took his doctorate at the Imperial
College of Science and Technology in
London in 1955 and has been conducting
research in geochemistry ever since.
He is a pioneer in the field of development of rapid methods of chemical
analysis of rocks and has applied his
talents to many geochemical problems.
Those who have worked with him know
and appreciate his messianic concern
with accuracy and woe betide the sloppy or untidy associate.

My three year association with Dr. Mercy at Lakehead University left me with a
high regard of his active and aggressive leadership.
In the face of overwhelming
difficulties he built up a faculty and facility of which any geology department
could be proud.
It is therefore with great pleasure that I dedicate this first volume to him
and I urge all who follow to strive for the high standard he sets and to continue
in this admirable enterprise.

James L. Talbot 3 Chairman 3
Department of Geology 3
University of Montana.

3

�:

V'
The production of this Geology Year Book is a major achievement by the geology students of
Lakehead University and I congratulate them for showing the initiative, energy, tenacity and the
many other qualities needed for the successful completion of their project.
The Department of Geology grew out of a Mining Technology program which had been given since
The Department, in its present form, is but
the early days of the Lakehead Technical Institute.
four years old and our first group of B.Sc. Honours students is preparing for graduation this May.

Our present teaching programs are as diversified as possible and are designed to give students
Thus we have
the maximum opportunity to choose directions in which they may develop their talents.
programs of study of Geology with Chemistry, Geology with Physics and Geology with Economics. We
believe that these programs can give students the education and experience needed to enter the whole
range of mining and petroleum industries as well as providing the academic basis for going on to
graduate schools.
The principal research activities of the Department are concentrated in two areas: a limnogeological reconnaissance survey of the Canadian portion of Lake Superior which is supported by
contracts negotiated with the Canada Centre for Inland Waters; and a multidisciplinary investigation
of a continuous section of midwest Superior Province crust, from Shebandowan to Pickle Crow, which
crosses five juxtaposed Archean belts. This latter research involves the close cooperation of
members of the Department with a group of geophysicists and geologists at the University of Toronto.
In this fourth year of the life of the Department I see that we are developing teaching and
research programs of good academic quality. We have a faculty and staff who are hard-working
persons dedicated to the pursuit of the earth sciences. But when all is said and done, it is
the quality of the students which will demonstrate to the outside world the nature of this
Department. You young men and women are our ambassadors. Yours are the talents which will make
the reputation of our Department known and respected.
In the production of this Year Book you
are showing that you are a group of people with a lively interest in and concern for your chosen
profession.
Good luck to you all.

I
Edward Mercy,
CHAIRMAN,
GEOLOGY DEPARTMENT.

MANUFACTURING
GEOPHYSICAL EQUIPMENT

Oil

Magnetometers, Ground Electromagnetics, Induced
SpectroPolarization Systems, Airborne E.M.,
Emano Mercury Detection
meters, Resistivity
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you

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For

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we
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THROUGHOUT THE

WORLD

�Dr. E« A. Ross, Dean of Science, Lakehead University

It is a pleasure to write this short address to the Geology Club of Lakehead University.
I
heartily commend the editor, Juris Zdanovskis, co-editor Patrick Fung, and photographers on their
enthusiastic enterprise in producing this Year Book. I believe it is the first of its kind to be
produced by any of the Students’ Clubs in Departments of the Faculty of Science, and the Department
of Geology should be justly proud of this agreeable achievement.

The significant role played by geologists in the discovery and development of the resources of
Canada is marked by history and yet my belief is that the best is still to come. Reference to the
Science Council of Canada Report No. 7 on the Earth Sciences would amply justify the tenor of that
statement.
The future prospects of exciting and creative work in geology, geophysics, geochemistry
and the other earth sciences must appeal to many of our brighter students who are oriented towards
the scientific disciplines. Many promising careers are and will be available to graduates in
research, development, consulting, management and so on.

Of course, a successful study of geology means continuous hard work, but when was any worthwhile
success or achievement obtained without such effort? Since, in Pantin's terms, geology is an
'unrestricted' science, the graduate geologist must and does have a wider knowledge and appreciation
of the other sciences than his colleagues in neighbouring disciplines with the possible exception
of the biologist.
I firmly believe that students of geology have chosen their subject wisely.
rewards will be many.

Go to it and your

To the members of the Geology Club of Lakehead University, I wish every accomplishment in the
future and extend my strongest hopes and support for the success of this excellent Year Book.

R. A. Ross

Dean of Science

5

�:

It will be appropriate hor me to gtve
G eology Club In our Firs 1 Geology VeaA Book.

a.

brieh reviejw on the short history

oft

oua

Oua University is young and oua club is still youngeA. But: its activities aAe
last as varied and plentiful and oua enthusiasm just as high as any. The loosely established
Precambrian Club maAked the ilut attempt by the students to organize a club hor the Geology
Department.
But it war In 1968 that the club war fatArt o ^totally ertabltrhed undeA the name
oh Lakehead University Geology Club.
The executive ion the three years oh the. club’r history
have been:
1 968-69
President:
Lou Covello
'

Secretary /Treasurer:
1

1

969 nc

President:

970/71

Secretary /T rear urer:
Vret tdent

Vhil Walhord

Veter Vans tone
Joe Kararda

Patrick Fung

Secretary /Treasurer:
J writ, Idanovskis
When h-itrl established three yearr ago, club actlvttler were limited to gatherlngr
In the recohd year, It began to
oh rtudentr, virltr to miner and varlour f^c&amp;Ed trlpr.
participate In external actlvttler Including correspondence with other university Departments
and geological organizations
It also rent the httsl group oh representatives to the First
Central Canada University Geological Conherence in Ottawa University
The representatives
were:
Brian Clerihew, Roy Shegelski, Peter Uanrtone. This year, we also rent oua representatives to the Second Central Canada University Geological Conherence in Queen' r University.
Oua representatives were: Patrick Fung, Rick Middaugh, Roy Shelgerki
,

.

.

Next year, we are going to rend one student speaker to the 8th Western Inter
University Geological Conherence to be held in Manitoba in October, 1971. Also, we have had
some very distinguished geologists to be our guest speakers throughout this year. The names oh
these and. their topics are given in another part oh this Sear Book. It is an honour to have
them to come and visit us.
I am sure all oh at have benehited by their lectures.
The idea oh a Geology VeaA Book war h^rr^ suggested by Dr. E. Mercy and Dr. J.
Mothersiii at the beginning oh the academic year and war supported by all the haaulty
members and rtudentr. The rtudentr h fl0m second year were particularly keen and enthusiastic
especially the Chieh Editor, Juris Idanovskis
But hall credit should be given to all
those who helped in producing the Vear Book and all those who have contributed to it.
.

We hope that it will be published every year in the hature.
May
As President I wish the Geology Club every possible success in the hature.
remind you that success depends up the enthusiasm and interest oh all the geology students.
We have made an- excellent beginning - I hope that you will continue this good work.
I

Patrick Fung,
President,
Geology Club.
6

'fa&amp;icJl pUtJj,

�The Geology Department is quite new to this University; it is small and not well
known to the rest of Canada; therefore the principal purpose of this first Year Book is to
advertise the Department and to make ourselves known.
The first talk of publication occurred at the beginning of the school year, but
little was done until a few weeks before Christmas, when a few of us began to consider where
the money would come from to pay for the publication. To my surprise, the response was
remarkable; the Geology Department was first to indicate mathematical figures that sounded
impressive. The Science Society, slow but sure was next in line. The rest of the money had
to come from advertising, a source which did not look too promising at first, because of our
late start.
The companies were agreeable and were sufficiently interested to pull us through
with the final cash resources.

Faced with a staff of bushwackers, who had little experience in publishing, we
worked slowly; but with all the problems we were still capable of putting out an excellent
book.
I should like to thank Dr. Edward Mercy, Chairman, Department of Geology, Lakehead
University, for his eager response in helping us to publish the book. Many thanks to the
Geology Secretary, Mrs. Jean Helliwell for her help with the business side, and her typing.
Without Sam Spivak's help and his artistic talent with the drafting pencil our advertising
would have been a mess. I enjoyed working with the staff that I had and hope to have them
back next year for the second publication.

If you, the reader, have any criticism of the book, please forward your remarks to
me and we shall try our best to improve the book.

Thanks to my staff for their time and patience.

Patrick Fung
Les Tihor
Paul Strandberg
Eric Brown
Elizabeth Hillary
Ron Wrigley
Ron Green
Dave Powers
Ralph Bullough

Juris
7

Co-editor
Photographer
Layout

Zdanovskis, Editor.

�with

compliments
from

the

faculty

of

science

lakehead

university

i

DEAN

8

R. A.

ROSS

�STONEWORTHY

!

COLLECT

SPECIMENS, DON'T

PRODUCE

'EM"

�Olivine diabase dyke in
the Coldwell complex.

Algal reef, Gunfiint
formation. Thunder
Bay Group, near
Schreiber, Ontario.
These reefs have grown
on boulders which form
the basal conglomerate
of the formation. They
contain blue-green
algae, and are, at
1.65 billion years,
one of the oldest
known life forms.

Thinly laminated limey mudstone beds,
Sibley Group, near Rossport, Ontaiio.
Note soft sediment folding.

10

�Stromatolites, Sibley Group,
Disraeli Lake, near Nipigon, Ontario.

Stromatolites grow in a near shore or
intertidal zone. These belong to the
genus Conophytum and are 1350 million
years old.

Mushroom shaped
concretion. Rove
formation, Tnunder
Bay group, near Pass
Lake, Ontario.
These concretions
have grown
diagenetically,
and contain possible
organic material.
They are composed
of cal cite

Tightly folded bands of
chert-magnetite iron formation
in an Algoman Iron Formation,
Kaministiquia, Ontario.

�Sam /V^

Diabase dredged close to the M.A.R.
A rough intersertal structure is formed by
coarse microlites of plagioalase and
interstitial pyroxene. Probably belonging to
a thick flow, or a shallow sill.
(45 N on the Mid Atlantic Ridge, 1200 fins)

Chromite opaque grains, within a
serpent ini zed ultrabasic lock. In tne
cavities of the chromite some lelics of
primary olivine and pyroxene may be found.
The fractures in the chromite grains indicate
a serpentinization of the surrounding rock
with a slight increase in volume.
(45 N, Mid Atlantic Ridge)

A quickly chilled basalt, with radiating
thin microlites of feldspar, within an
opaque hematite stained glassy matrix.
Small angular grains of olivine are visible.
Note the hollow transversal sections of the
feldspatic microlite.
(From 45 N, Mid Atlantic Ridge, 1200 fms deep]

This specimen is a serpentinized dunite. A
tiny fracture in the specimen was invaded
by a fora minifera ooze, and the walls of
the fissure are coated by dendritic Mn and Re
oxides.
(From 45 N, on the Mid Atlantic Ridge,
1300 fms dep)
12

��.

Dr. Edward Mercy, B.Sc., Ph.D.

,

D.I.C.

Academic Background
Lecturer in Geology: Imperial College of
Science and Technology, London, England.

Lecturer in Geology, later Senior Lecturer
in Geology, University of Edinburgh, Scotland.

Professor of Geology and Chairman of the
Department, Lakehead University.

Research
Geochemistry of a Granite Series in Donegal, Ireland.
Geochemistry and mineralogy of gamet-peridotites and
eclogites from Norway, S. Europe and S. Africa.
Geochemistry and mineralogy of spinel-peridotites from
the Lac de Lherz region of the Pyrenees.
Geochemical studies of plutonic and volcanic rocks in
Northwestern Ontario.

CURRENT RESEARCH
The mineralogical nature of the mantle of the earth can be deduced in three
ways - by considering what known earth materials fit the determined geophysical
parameters (such as pressure, temperature, density, value of the gravitational
constant, the velocities of seismic waves, and others), by relating the known
chemical compositions of basaltic magmas to possible mantle compositions which
could produce such lavas by partial or complete melting processes, and by studying the mineralogy and chemistry of rocks, emplaced at high levels in the crust,
which might represent unaltered mantle squeezed up into the crust by tectonic
processes or brought up as xenoliths in magmas.

There is general agreement that the uppermost part of the mantle and at
least some part of the lower crust is made up of the assemblage: olivine +
orthopyroxene + clinopyroxene + spinel = spinel lherzolite. This is considered to be representative of granulite facies conditions in contrast to the
eclogite facies conditions of the deeper parts of the mantle which is represented
by the assemblage:
olivine + orthopyroxene + clinopyroxene + garnet = garnet
lherzolite. Natural materials which have the appropriate properties are the
spinel-lherzolite xenoliths occurring in basaltic lava flows and the garnetlherzolite xenoliths in the Kimberlite diatremes of South Africa. Another type
is represented by the series of small tectonic intrusions of spinel-lherzolite
which outcrop in the French Pyrenees

A period of field work based at the beautiful town of Foix enabled me to
make a detailed study of what Lacroix described as the type lherzolite. This
occurs at a height of 1300 metres o.d. at the Etang de Lers as a tectonic
intrusion into tightly folded and strongly metamorphosed Mesozoic rocks. The
lherzolite contains 45-85% by volume of olivine, 10-35% orthopyroxene, 5-20%
diopside, and 1-6% spinel. These differences in mineralogical composition are
caused by the layered structure of the lherzolite.
The main point of lherzolite work is an understanding of the chemistry of
the lherzolites and particularly the distribution of elements such as nickel
and chromium between the various mineral phases.
Such data can lead to knowledge
of the conditions of equilibration amongst the phases and may enable one, in
comparison with a very great amount of published work, to establish models for
the chemistry of the upper mantle.

Edward Mercy
14

�Dr. J. Mothersill, B.Sc, (Physics) Carleton;

(Geological Engineering) Queen's;

B.Sc.
Ph.D. Queen's .

Background

Exploration Geologist for Standard Oil (N.J.)
Senior Geologist for Mobil International Oil Co.

Exploring for petroleum in Turkey, Nigeria, France
and Colombia.

LIMNOGEOLOGICAL STUDIES OF THE EASTERN PART OF THE LAKE SUPERIOR BASIN
The bottom topography of the eastern part of the Lake Superior basin consists of a lake-shelf two
to four miles wide and a series of north-south aligned, topographical deeps and highs three to four
miles wide lakeward, which is in marked contrast to the east-northeast and east-southeast trends
of the onshore Precambrian rocks.
The temperature of the bottom sediments is related to waterdepth.
The high pH values of the bottom sediments in Goulais Bay and Batchawana Bay appear to be
caused by the alkaline waters of the Goulais and Batchawana rivers respectively. The pH measurements of the bottom sediments elsewhere in the area of study do not appear to be related to
either water-depth or to the lake-bottom sedimentary types.
The Recent sand deposition is restricted to the lake-shelf and to the offshore topographical high
areas. Based on grain-size analyses the sands of the topographical highs are normally coarsergrained and better sorted than the sands of the adjacent lake-shelf area suggesting stronger
current action offshore.
In addition the sands of these two environments can be differentiated
on the basis of total heavy mineral content as the sands of the topographical highs never contain
more than 3»1 per cent heavy minerals whereas the sands of the lake-shelf area may contain from
4.1 to 26.0 per cent heavy minerals.
The main area of provenance for the sands would appear to
be the rocks along the shoreline and the drainage area of the eastern Lake Superior basin.
The
reason for the relative decrease in the percentage of heavy minerals present along the topographical highs would appear to be that most heavy minerals are unstable in a fresh water environment
and therefore would tend to be chemically decomposed before being transported to the offshore
topographical high areas.

The sands south of Coppermine Point are generally coarser-grained, better sorted and less
positively skewed than the sands north of Coppermine Point regardless of environment of deposition.
This is probably the result of stronger current action along the shallower waters of the topographical highs and lake-shelf area south of Coppermine Point. The occurrence of a thicker sand
sequence in progressively shallower water from north to south across the area of study could be
related to the post-glacial isostatic tilting of the Lake Superior basin to the southwest as the
Michipicoten area has been raised 20 meters relative to the Sault Ste. Marie area since the
Nipissing stage (Farrand, i960 ).
The Recent sediments in the central parts of Batchawana and Goulais Bay and in the offshore
topographical lows consist of coarse silts to coarse clays. These Recent silt-clays form a
consistent sequence of the following three units: an upper thin veneer (&lt; 4 cm. ) of coarse to very
fine-grained dark yellowish brown silt; an intermediate, relatively thin (2-12 cm.), unit consisting of olive gray, fine-grained silt to coarse-grained clay; a lower thick unit of coarse to
very fine-grained, dark yellowish brown silt.
The thickness of this sequence is greatest in the
central parts of the topographical deeps where it is in excess of 180 cm. thick. The mineralogical
composition of the three units is very similar and consists of orthoclase, microcline, quartz,
15

�The difference in colour is probablychlorite, illite and an interbedding of chlorite and illite.
caused by the higher oxidation state of the dark yellowish brown silts.

Varved sediments, probably of Pleistocene age, underlie the Recent sediments in the area of study.
North of Coppermine Point the varved sediments are greenish gray in colour whereas to the south
The mineralogical
of Coppermine Point the varves have been oxidized to pale brown in colour.
composition of the varved sediments consists of orthoclase, microcline, quartz, chlorite, illite,
an interbedding of chlorite and illite, dolomite and calcite. It was noted that there is a
decrease in the percentage of calcite in the varved sediments northward of St. Mary's River.

JOHN
LAKE

S.

MOTHERSILL

SUPERIOR

LIMNOGEOLOGICAL

STUDIES

BASIN.

16

OF THE

EASTERN

PART

OF

THE

�Dr. Henri Loubat
Geological Engineer, PhD., Geneva
Assistant Professor, Lakehead University

Petrology
I became particularly attracted by petrology in 19ol when I found the
opportunity of studying a set of metamorphic rocks from California. These rocks
belonged to the glaucophane-schist and eclogite facies of metamorphism. At that
time, I was fascinated by two problems exhibited by these classic Californian
types: the process of diaphtoresis and the phenomenon of converging facies.
,

The "glaucophane-schist" may be due to a particular regional metamorphism
acting on greywackes and ophiolites; but frequently it results from a retrograde
process of modification from a high degree of metamorphism (amphibolite or
eclogite) toward lower degrees of alteration. Both these glaucophane-bearing
types are to be found, closely associated, in California, and they exemplify very
well the retroinorphosis diaphthoresis) and facies "convergence". It is easy to
realize the interest of the study of those facies, if we know that eclogite
themselves are not always considered as metamorphic rocks....
(

Soon after, receiving a grant from the University of Geneva I studied
briefly greenstones, sediments and serpentines from Cuba. The degree of
alteration of my samples was somewhat discouraging for a sucessful petrographical
and geochemical investigation, but this was a first contact with igneous
submarine rocks.

During the next four years my main petrographic activity was devoted to
surveying the Versoyen region - this area of the Alps is geologically very
attractive. We should know that the Alps are subdivized longitudinally by a major
tectonic thrust plane, the trace of which is called the "Pennic front thrust".
This line runs parallel to the chain, subdivizing it into two equal bands: the
"internal Alps" (toward Italy) and the "external Alps" (toward France and
Switzerland). The former is very rich in ophiolites, strongly metamorphic and
intensely disturbed by the tectonic. The latter is not metamorphic, lacking
ophiolites, and gently folded. The Versoyen, which is located exactly on the
border between France and Italy, is the last ophiolitic area we could find when
leaving the internal Alps going toward France, ’with this marginal location, this
area offers the weakest degree of metamorphism we could have in the Alps for
submarine volcanic rocks.
A study based on field, microscopic and chemical investigations leads to
the following conclusions:
'We have there a well-preserved submarine volcanic complex composed of the piling
of various related units; at the bottom, along with slabs of aplitic granites and
gneiss (fragments of the Alpine basement?), thin layers of serpentinites . Above,
thick lenses of diff erenciated gabbros; still above, a set of sills, inter-bedded
with black schists. At the top, an enormous amount of pillow-lavas. This rather
logical sequence so well known by anglo-saxon geologists, was never recognized
before anywhere in the Alps, although it is quite probable that it is actuall'
omnipresent, but was always disturbed by complex diastrophism.
17

�o

Moreover there was an interesting point about the metamorphism of the
volcanic system: the intensity of metamorphism was steadily decreasing from the
I suggested an eventual
bottom to the top (very weakly metamorphic pillows)
direct relationsnip between the depth of the crustal segment and a kind of
late-magmatic auto alteration (deuteric alteration).
.

These are the reasons why I remain personally interested in the results of
dredging operations, close to any mid-oceanic ridge. If there were some
metamorphic rocks already there, they may well be attributed to some process of
alteration of that kind.
As soon as you are occupied by such questions, generally many other
interesting problems arise. Studying recently, in collaboration with the Bedford
Canadian Oceanic Institute, a set of dredged specimens, I momentarily shift
toward another topic of interest: the origin of the dredged serpentinized ultrabic
fragments. Among many interesting and mysterious facts, we found evidence of an
intense pre-serpentinization cataclasis, probably due to a creeping process at the
base of the crust, and presumably related to the oceanic floor spreading. Many
N. lat. on the Mid Atlantic Ridge are still
metamorphic specimens from
waiting for an investigation; we may say already that they uniformly belong to the
green schist facies only.
It is fascinating to meet, near Thunder Bay, in the heart of the Canadian
Shield, greenstone belts showing perfectly preserved relics of submarine basic
lavas, exactly similar to the one formed very recently. It is extremely promising
to compare their detailed petrological properties, with those recent equivalent
rocks, because we may suppose some kind of difference between now and 3 billion
years ago in the superficial environment and in the relations between continents,
oceanic crust and mantle. In this comparison, as a petrologist, I foresee the
possibility of detecting an evolution of the earth's crust, evolution about which
we do not even have a serious hypothetical model yet. The geology school at
Lakehead has therefore, a wonderful field of investigations for a long and
sucessful future

BONGARD

LESLIE

&amp;

GO.

LTD.

204 ARTHUR ST.
THUNDER BAY (P), ONT.

STOCKBROKERS
BOND DEALERS
MUTUAL FUNDS
TELEPHONE

D. F.

W. N.
S.
J.

BARON
AUBRY

MALINOSKI
M.

SCOTT

344-6618

MGR.

�Dr. James M. Franklin, B.Sc.

(Carleton);

(Carleton);

M.Sc.

Ph.D. (Western) .

Background
Geologist for G.S.C.
Assistant Professor, Lakehead University-

Research

Metallogeny of the Lake Superior Crustal Traverse,
Shebandowan to Pickle Lake
Origin of low temperature silver deposits, Thunder
Bay area

Stratigraphy of the Sibley Group, Thunder Bay
District

Metallogeny, Its Concepts and Uses
Two concepts of metallogenesis are (l) the genesis of a single metal in a variety of geological
environments, and (2) the examination of all mineral deposits within a geologically or geographically defined region.
The "single metal" concept does not facilitate documentation of variations in mode of occurrence
with time, and may preclude comparison or integration of genetic ideas related to one metal with
with those related to another. This concept does, however, allow for complete examination of the
chemistry of concentration of a metal in all geological processes. For example, Gross (1965) in
his study of iron deposits, is able to document the processes operative in concentrating iron
in igneous (iron-titanium deposits associated with Grenville anorthosites), metamorphic (contact
meta somatic deposits of Vancouver Island) and sedimentary (Algoma, Superior and Minette type
deposits) bodies. Such a study contributes much to fundamental geochemistry, but may, in certain
circumstances, be of less significance in deposit exploration. For example, in searching for
copper, the exact nature of the chemical control on deposition of the metal is less important than
the stage of development of a eugeocyncline or facies of cratonic cover sediments affiliated with
copper deposition. Recognition of the appropriate lithofacies associated with a deposit is a
fundamental factor in delineating new areas of exploration.

The second metallogenetic concept involves examination of variations in mineral deposit type within
litho stratigraphic or petrogenetic province. Basically an accurate interpretation of source and time of deposition of mineral deposits is integrated with a regional
tectonic history including geosynclinal and post-orogenic evolution.
Clearly, a prime difficulty
in such a study is. selecting useful co-incident geographic and geologic limits. All lithological
and structural variations in any time—unit should be included within the geographic bounds of the
study.
The area must have adequately outlined mineral deposit genesis, paleogeographic and
tectonic reconstruction.

a time-stratigraphic,

Convenient geologic limits might be set by systemic boundaries and orogenic events. For example,
the Aphebian era is defined at its initiation by the Kenoran orogeny, and at its end by the
Penokean and Hudsonian orogeny. The Helikian era is defined by the latter orogenies at its
inception, but the termination of dominant continental volcanism and sedimentation at its end.
Together these eras include many conventional tectonic elements. The problem is to select an
area in which the complete geosynclinal, mountain building, and continental deposition events
are preserved.
The Lake Superior and Central Labrador areas meet these requirements. A
metallogenic scheme for the former region is outlined in Table 1.

19

�.

.

.

.

Two uses of such a scheme might be found in mineral deposit exploration and research into earlycrustal conditions. For example, the exploration geologist may not have been aware of the
possibility of "breccia-pipe" porpbyrycopper deposits associated with Neohelikian rocks of the
Lake Superior area. Examination of available maps indicates the presence of many crypto-volcanic
features; more deposits of the Tribag type might be found at appropriate structural loci.
Metallogeny might also be useful as an indicator of a specific tectonic stage. For example, if
anomalous concentrations of molybdenum are found only in post-orogenic, "high level" salic
intrusive rocks, then the presence of this metal in certain Archean granite may suggest that
these granites formed much later than the predominant volcanic rocks, 1 in a post-island arc,
continental setting. We may thus investigate the possibility of two igneous events in the
Archean which may have occurred at widely separated times.

Metallogeny of Proterozoic Rocks in the Lake Superior Area
Sedimentary and
Effusive Rock

Tectonic
Stage

Time m.y.

coarse continental
sediments, fine.
lamellar interflow
sediments (after
in situ' weathering of volcanics).
Flood basalt, minor
rhyolite

1000

'

Intrusive
Rock

Structures

minor, alkalic
complexes carbonatite. Major
layered gabbroic
bodies, diabase
sheets

Cratonic faulting and tilting
due to deep
fracturing.

Syngenetic Deposits

a) Cu

in alkali

Multiple Stage Deposits
Source Bed External forces,
for
applied, formation
of deposits
Cu

bodies
b) Cu-Ni in layered

mafic bodies.
c) Cu in basalt.
d) Cu-Mo in breccia

pipes (Tribag)
possibly as gaseous effusions.

tilting allows
updlp migration,
precipitation of
Pb-Zn at
structural trap.
b) Mafic intrusive
sills and dykes
cause remobilization of Ag to
structural loci
formed due to
contemporaneous
cratonic faulta)

ing.

interflow
sediments

c) Cu to

Continental red
bed sedimentation

1350

none

Pb-Zn-Ba
in red
beds

uplift, consequent weathering

granite
granodiorite
pegmatites

Cratonic

1650

Protogeosynclinal

blackshale, iron
formation, minor
basalt, limestone,
greyvacke.

Protobasin

orthoquartzite,
cgl, greyvacke

2100

deformation.
simple folding,
faulting. Metamorphism in
deepest parts
of basin, minor
anatexis.

deeper basin
sediment added
at same rate as
basinal subsidence.

minor
gabbro

(Uranium, Elliot
intermontain
*
basins, shallow Lake)
rapid weathering
transport in
streams
-

2500
NOTE:

Brackets indicate deposits not in region of this study.

1 -

Armbrust, 1969

^ -

James et al.

3

Roscoe, 1969

-

,

Iron
(minor Cu in
gabbro)^

1968

20

Ag in
shale

�Dr. K. Chakraborty, M.Sc.

(Jad»);

Ph.D. (l»I«T.

)

Assistant Professor, Lakehead University

A Statistical Study of Crystal Contacts Across a Segregated

Hornblende Vein in Amphibolite and its Implication
The pattern of spatial distribution of crystals in rocks depends on the energies of crystal
contacts and entropy of distribution.
The stable equilibrium patterns possess minimum distributional free energy. For a linear unidimensional system consisting of equal numbers of A and B
crystals of the same size, the distributional free energy can be expressed as

F =

i

n P( u

M

+ U BB - 2Uab ) + nUAB + nkT [p log

(-gp)

+ (l - p) log(l - p)]

= energy of A-B contact, etc., and p = probability of A having another A as neighbour.
where U
Thus, for given contact energies, the value of p corresponding to the minimum of F would determine
the spatial distribution of crystals in the rocks.

The energies associated with different types of crystal contacts in natural rocks are unknown.
However, if p can be determined, it might be possible to decipher the relative energies of the
crystal contacts. A possible way to determine p is to carefully evaluate the frequencies of
different crystal contacts in a given rock. Frequencies of contacts depend on the preferred
crystal associations as well as on the modal percentage of the minerals and crystal sizes. By
suitable statistical device (Markov Chain) the frequency of crystal contacts only due to preferred
crystal association can be evaluated. Crystal association during crystallization of a rock is
governed by other factors apart from contact energies. Hence evaluation of contact energies
would be plausible where rearrangement of initial crystal association is apparent.

An attempt has been made to evaluate relative energies of hornblende-hornblende, plagioclaseplagioclase and homblende-plagioclase contacts from a specimen of amphibolite (hornblende and
plagioclase together make up more than 90/o by volume). The specimen contains a differentiated
zone consisting of a hornblende vein bordered by a feldspathic aureole.
It has been concluded
elsewhere that the differentiation is later than the crystallization of the amphibolite.
Frequencies of crystal contacts across the differentiated zone are analyzed statistically
employing Markov Chain concept. It is observed that homblende-plagioclase contacts are minimum
The
in the differentiated zone and gradually increase and assume maximum value away from it.
reverse is true for hornblende-hornblende and plagioclase-plagioclase contacts. Thus the
distribution patterns of crystals in the amphibolite away from, adjacent to and within the
differentiated zone are ordered, random and segregated respectively. This suggests that
segregational pattern possesses minimum distributional free energy for this system which is
possible if the mean energy of hornblende-hornblende and plagioclase-plagioclase contacts is
less than the energy of homblende-plagioclase contact.

21

�Analysis of Material Balance in Segregated Bodies
Existence of material balance is one of the most convincing evidences in favour of segregational
origin of the differentiated features like veins or lenses of mineral "concentrates" bordered by
characteristic "aureoles". Analysis of material balance is therefore crucially important and it
cannot be overemphasized that the methods employed for such analysis ought to be reliable as well
as capable of revealing the true state of balance within the differentiated bodies.

By use of spherical and triaxial ellipsoidal models of segregation the reliability of the methods
commonly used for balance analysis are tested. It is demonstrated that none of them can yield
correct results. The reason for this is that these methods do not take the true volume ratio
This volume ratio is an indispensable factor
of the "concentrate" and "aureole" into account.
for correct balance analysis. Accordingly, modified procedures to evaluate the state of balance
are suggested. Determination of the above mentioned volume ratio in natural specimens is
extremely difficult and imposes severe restrictions on the scope of balance analysis.
The state of balance across a hornblende vein surrounded by a feldspathic aureole has been determined by the suggested method as well as by one of the existing methods for a comparative
evaluation of their reliabilities. The results obtained by the suggested methods show that
material balance exists, thus indicating the segregational origin of the vein. This agrees well
with the conclusion derived from mineralogical and chemical evidences. But, as predicted from the
model studies, the existing method shows a lack of material balance across the vein.

GRADUATE TO FALCONBRIDGE
Geologists, Geophysicists, Geochemists, Mineralogists

Mining

SEVEN KING STREET EAST,
TORONTO 210, CANADA

and

Electronic

Technologists

FALCONBRIDGE NICKEL MINES LIMITED
23 TOMLINSON BLOCK
sa n. Cumberland st. -thunder bay. ont.

22

�Mr. R. Bennett. Honours Practical Geology,
Heriot Watt College. Edinburgh, Scotland
.

Background

:

Chief Laboratory Technician, 1936-1967
The Grant Institute of Geology,
University of Edinburgh.
Researching many kinds of technical
approaches to Ph.D. studies.
Presently, Chief Laboratory Technician,
Lakehead University.

Thin Section Making with the Aid of
Araldite Epoxy Resin.
Araldite Epoxy (Resin 502, Hardener 956)has the ability to penetrate into the cracks and
cleavage planes of minerals and it will bond efficiently the angular particles of semi-consolidated sedimentary rocks, as well as recent sediments and soil samples.
The adhesive properties
of the Resin are such that it can be used as a mounting media, where such thermo-plastics as
"Lakeside 70" cannot be used or are not advisable due to the re-arrangement or twisting of the
surface to be mounted.

IGNEOUS

ROCKS

The following are some of the ways in which Araldite Resin was used in making thin sections
of serpentinites from the Atlantic Ridge of the Azores.
These rocks were very fragile and had
a coating of manganese over the whole or part of the sample.
The Preparation for the thin section:
Due to the fragmental nature of the sample, it was necessary to bond a part of it even
before attempting to cut it.
This is done by mixing Araldite Resin ( 10 parts of resin to
The SDecimens to be cut
2 parts hardener, by volume) in a thin-walled pliable polythene jar.
are placed in an oven set at 60 degree Centigrade until the surface is hot to the touch.

Remove from the oven and immerse the portion of the rock to be sectioned in the resin.
Return the polythene jar with the specimen to a vacuum oven and impregnate the sample.
When
the oven chamber starts to evacuate, the resin will start to froth.
This frothing is controlled
by periodical closing of the vacuum and slowly allowing the air to force the resin into the sample's
surface.
Repeat this procedure until it becomes apparent that there is sufficient penetration
of the resin into the surface of the sample, so that when cold, it can be cut without breaking.
The Cutting:
Remove the sample from its container.
A surrounding mass of excess resin is beneficial,
as it will preserve the outside edges of the sample.
If
Clamp the unimpregnated part in the cutting machine and cut off the required part.
the specimen is holding together, then cut a second slab for future work.
Wash the cut-off
part and examine it under the microscope.
Ensure that the surface cracks have been impregnated
and if not, dry the slab and return it to the oven to complete drying and warming of the surface
for coating with a fresh mix of resin.
If the slab is used, it may suffice to place it on the
plate to warm for surface coating.
Surface coat the slab with resin, impregnating it as before
if it was on the hot plate or in the oven.
Allow it to set, strip off any unwanted resin with
a razor blade while the slab is still hot, to save unnecessary grinding.

23

�:

When the sample is cold, trim to the size of a sli'de and grind to a very fine mounting
surface, using either coated carborundum paper (400, then 600 grit) or a glass plate with the
Wash the sample and ensure that the required surface is whole (not
same abrasive and water.
pitted) and even.
The Mounting:

Use the former if the surface
This can be done using Lakeside 70 or Araldite resin.
likely to twist and buckle when re-heated, which would cause an uneven mount.
If the resin is used as a mounting media,
The latter should be used if this is apt to happen.
press them
apply a small amount to each surface (the glass slide and the sample surface)
This
together to remove all the air and allow it to set at room temperature for 24 hours.
will allow the resin to set sufficiently for grinding.
is hard and not

,

The Thin Section:
Cut or grind the sample down to the first stage of transparency, using either
bonded wheel or the carborundum method.
It is now that
the silicates and the
to hand grind the now
desired, taking great

a

diamond

Due to the differences in structure of
the bonding shows its effect.
manganese crust to transmit ordinary light, it is therefore beneficial
thin section to completion on a glass plate with 600 grit or finer if
care to retain the complete surface area.

Having completed this stage to the required thickness, wash the section and dry it with
If the latter is used, trim the
tissue;
then remove the surplus Lakeside or Araldite.
outer edges leaving a small border around the section edge, but do not attempt to remove all
Clean
the Araldite from the thin section as this will result in the destruction of the sample.
Clean and cover a covering
the surrounding slide with a solvent such as chloroform or acetone.
slip with a reasonable amount of Canada Balsam, warm it on the hot plate until the Balsam flows
outward over the cover-slip, and in the meantime warm the surface of the thin section.
Do this
by holding it over the hotplate without touching it, and then laying the two surfaces together.
Remove the covered section from the hotplate, then carefully press down the cover-slip to remove
all the air.
Clean off the surplus Balsam with acetone and finally with chloroform.
a

If the thin section is too fragile to use heated Balsam, use Permount and allow to dry
This takes longer, but it helps to retain the structure of the section.

at room temperature.

SEDIMENTARY

ROCKS

The thin sectioning of sedimentary rocks such as sandstones, sandy shales, clay shales,
etc. can be difficult when their natural cementing media is a carbonate or some other material
(with the exception of silica).
It is therefore necessary to impregnate the rock with a
material that will act as a bonding substance to retain the grains and structure of the rock
in original form.
If the rock matrix is a carbonate, either calcite or dolomite, the action of the cutting
blade will tear away the carbonate, leaving many loose grains, and the stages of grinding prior
to mounting on the slide will have a similar effect, though not so harsh.
If the fine-ground
slab is washed down and dried, then examined under a binocular microscope, it will be observed
that the cleavage- planes of the carbonate have been irritated and are apt to be loose.
Therefore, when the slide mounting media is applied to the section slab, and the slide placed in
position, a gritty feeling will be observed.
The result is a thin section full of holes, due
to the fact that all the grain surfaces were not on an even plane.

If the same sandstone were impregnated with Araldite Epoxy Resin, all the grains as
well as the cleavage planes of the carbonate would be bonded together to create a solid
interior which can be thin-sectioned without any difficulty.
The same technique may be
applied to sandy shales and the fine laminations of shales.

Method
Cut the rock with a diamond blade to a thickness of no less than one quarter of an
Dry the slab and place it on
inch, as this will give a sufficient depth with which to work.
a Teflon plate (Use Teflon because of its self- lubricating properties as well as its high
melting point) and put the unit in a vacuum oven and bring it to 60 degrees Centigrade.

24

�;

:

Mix a small batch of Araldite Resin (such as 20 ml. of resin to 4 ml. of hardener),
Remove the Teflon
stir it well and leave it standing until the mass of air bubbles is out.
plate and the slab from the oven and quickly apply a surface coat of the resin to the slab,
When the resin has stopped frothing,
and then return it to the oven and re-evacuate the air.
The inrush of air will force the resin
close the vacuum valve and slowly open the air vent.
Leave the unit in the oven to cure for two hours and then allow it to cool to
into the slab.
Remove the slab from the Teflon plate and cut it to the size required for
room temoerature.
The grinding for mounting is the same as for a hard rock section.
thin section.
The mounting media should be Lakeside 70 and the sectioning is the same as before with
The covering
the exception that the sandstone can be machined thinner, saving hand grinding.
is the same as before.

THE IMPREGNATION OF RECENT SEDIMENTS

by

a

The following report is on the technical procedure of making
micro-polished surface of a recent fine grained sediment.

a

thin section followed

The sediments which are wet when collected in core form are cut along their length to
The selected parts are removed and dried out slowly to
expose the variation in deposition.
prevent excessive shrinkage and to minimize the number of cracks.

Stage

I

This is done on
The first stage is to grind a flat surface of the selected sample.
dry abrasive paper of 400 grit, and then on 600 grit until the surface is flat, blowing off
any excess with a compressed air jet.
Stage

1 1

The impregnation media is Araldite Epoxy (Resin 502 Hardener 956) (a mixture of 10 parts
Teflon should be used for the mould, as it is a self- lubricating
resin to two parts hardener).
plastic which does not require any releasing agents.
It is convenient to have circular rings
of varying depths and diameters - these rings are placed on a Teflon plate (one quarter of an
inch thick) to prevent bending.
The ring is held in place on the plate with a thin layer of
silicon grease, which prevents leakage from the mould.
Place the sample in the mould, prepare
the resin and let is stand to allow any excess air to come to the surface.
Wet the surface of
the specimen with Methyl Ethyl Ketone, (a resin thinner which invades finer layers, allowing the
resin to better impregnate the sample).

Pour the resin into the mould so that it just covers the sample, and then put the unit
in the vacuum oven and start to evacuate the chamber.
At 15 pounds pressure, the resin will
start to froth.
Do not allow it to overflow the mould, and to prevent this close the vacuum
control valve and slowly open the vent.
The inrush of air will start the impregnation of the
sample, a repetition of this process should be done until there is no bubbling under the vacuum.
Close the vacuum control, switch off the pump and open the vent slowly.
When the vacuum is
released, set the oven heater at 60 degrees Centigrade and allow it to cure for two or more hours.
Remove the unit from the oven and allow it to cool.
Separate the ring from the Teflon
plate and press out the sample.
The method of preparation for thin section is similar to that
of a sedimentary rock, with several exceptions.
The surface to be mounted on the slide must be
on an even plane with the surrounding resin so that there is no relief between the two.
The
only way to obtain a flat even surface, if the sediment does not fine grind flat, is by repeated
surface impregnation, and careful fine grinding.

Use a fresh mix of resin as a mounting cement.
Apply a little to the slide and to
the fine surface of the sample and press them together.
Leave it to set for at least 24 hours.
The now thin section is ground to its proper thickness, after machining as before, on a wet
glass plate using 1000 Carborundum, clean and cover with thinned Balsam or Permount.
The Polished Surface

is

The preparation is the same as for the thin section, with the exception that the sample
moulded in a bakelite ring especially made for the DUrner Polishing Machine.

The most important part of this technique is to obtain a hardened flat surface prior
To obtain this surface, it is necessary to carefully dry grind the
to mechanical polishing.
specimen on fine abrasive paper, with frequent examination under the binocular microscope, to
25

�: :

ensure that a complete mineral surface is present - not one with a microlayer of resin over it.
When this is done, and the edges of the mould have been bevelled, it is now ready for the
polishing laps.
Lap

I

After switching on the
The first polishing is done with 6 micron diamond powder.
An even smear of mineral oil,
lapping machine, clean the lap with acetone and a tissue.
"liquid paraffin" is apolied to the lap, and a small "finger tip" of a 6 micron-diamond is
run over the lap.

The time for the first stage varies as to
Stop the lap and fit tne specimens to it.
Otherwise, if the lap is
the texture of the specimen, so it is decided by trial and error.
running well, one hour should suffice before the first microscopic examination.
As the particles of the metallic oxides and sulphides are very small it is advisable
If the pits are
to use medium to high magnification to get a fair reading on the surfaces.
still present, clean the lap, recharge and rotate for a further hour.

Lap II:

Repeat the same process for the second grade of diamond (l-3 micron) to get more
Here the surface should really show a polish, with small polishing scratches
definite results.
on the ore particles.
Lap III:
The final polish is done with 0-2 micron diamond and a small amount of oil, enough only
to lubricate the lap and avoid "snatching" and ejection off the lap.

When the surface is finished, clean it and store in a dry container to prevent moisture
affecting the fine sulphides and thus spoiling the surface.

I

llustrations

A.

Microphotograph:

B.

Thin section plain light 2.5X
M n bed.
showing (a)
(b)

Microphotograph:
Polished Section plain light 40X

Grainy Pyrite.

Fe bed.

26

�TECHNICAL &amp; SECRETARIAL
STAFF

27

�—
The

late

played a

Hugh M. Roberts
vital

part

—

the great

American Geologist whose faith and knowledge
the Steep Rock Iron Range, said

the development of

in

,

"THE SCIENCE OF GEOLOGY IS ONE ATTEMPT TO ESCAPE BEING LOCALIZED.
WE ENDEAVOUR BY MEANS OF THIS SCIENCE TO REACH OUT BY OBSERVING
AND INTERPRETING OUR SURROUNDINGS. WE LIVE IN THE MIDST OF TWO
INFINITIES, ONE THAT REACHES INTO THE DEPTHS OF A MICROSCOPIC CRYSTAL,
THE OTHER WE BEHOLD IN A MOUNTAIN RANGE AND IN THE IMMEASURABLE
"
DEPTHS OF THE STARRY HEAVENS

WE WISH THE LAKEHEAD

UNIVERSITY GEOLOGY

CLUB EVERY SUCCESS

STEEP ROCK IRON MINES, LTD.
ATIKOKAN - ONTARIO

The

Mining

Patino

an expanding mining
with

We may

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and exploration company

world - wide interests

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28

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want

�AFTER A WHILE IT ALL BEGINS
TO LOOK THE SAME.
II

�All the comforts of home -

Thax-'s what I call a good

cup of coffee]]

And when I strike oil, wnat
do I do then]

Okay, what else do we need
besides cigarettes and
crackers
oh-oh, we
forgot the toilet paper]

—

Uh - sir, we forgot the pilot
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—

30

�31

��II

�Modern mining exploration requires more
than a pick and a pan
Cominco

offers world markets an increasingly diversified product
range which requires the successful development of new sources
of metals and industrial minerals. Extensive and aggressive
is required to meet future needs and replace the ore
which Cominco is currently mining at approximately seven million
tons each year. To accomplish this Cominco spends several

exploration

million dollars annually

in

exploration programs

in

Canada, the

United States and overseas.

ENplorabion

34

TCommco

�dij

\

:
*

^
Jflj

1IS 1
l+'ld'&amp;jfi

fat T'

:*T3

�Roy Shegelski
Experience: Economic Geology
Limnology - 1969-70
Canada Centre for Inland Waters

GENERAL STRATIGRAPHY AND Fe/Mn BEARING BEDS OF THE SEDIMENTS OF THUNDER
BAY, LAKE SUPERIOR
R.

Shegelski

J.

In the summer of 1970, a reconnaissance survey was done of the bottom sediments of Thunder
Bay.
This was generally done with a Boston Whaler using a Phleger corer and a Ponar grab sampler
and 147 sample points were done in this manner.
Three sonar traverses were also made in the Bay.

Samples were brought back to the laboratory for analysis. Cores were split and lithologies
were recorded.
Samples from cores were analysed by x-ray diffractometer, thin and polished
sections were made of various parts and certain layers were analysed for iron and manganese.
Results of analyses indicate that the sediments in Thunder Bay can be divided into five
categories.
Varved Clay.
Weathered Varved Clay.
Intermediate Clay.
Upper
(1)
(2)
(3)
(4)
Deltaic Sediment.
Upper Trough Sediment. Through correlation of the cores and sonar runs,
(5)
the stratigraphy has been established as such.
The Varved Clay is the oldest, the Weathered
and Intermediate Clays are the second oldest and the Upper Sediments are the youngest and overlies the previous types.
An areal distribution is shown in the accompanying map.
Results of the iron and manganese analyses indicate that the Upper Sediments contain
anomalously high concentrations of iron and manganese.
It has been proposed that upward
migration of connate waters rich in iron and manganese has produced highly concentrated
layers of iron and manganese near the top of the Upper Sediments.
The proposed mechanisms of
concentration are precipitation, burial subsequent resolution and upward migration causing
redeposition at an appropriate Eh, (pH) interface.

AND

CONGRATULATIONS
to

the

M. W. Bartley

BEST WISHES

Graduates

&amp;

Associates Ltd.

Geologists

204

Toronto - Dominion Bank Bldg.
Thunder Bay, Ontario

36

��Copper and Molybdenum
Distribution in the Soils
of the Gavin Lake
Copper-Molybdenum Property,
British Columbia
By Peter J. Vanstone

The Gavin Lake property is
located in south central British
Columbia, about 25 miles east of
McLeese Lake. The property lies on the
eastern side of the Quesnel Trough,
which is a trough of Mesozoic strata
flanked by older Paleozoic and
Proterozoic strata.

Geologically, the property
consists of two main rock groups:
volcanic rocks, which include
sediments of volcanic derivation, and
porphyritic quartz monzonite. The
volcanic sediments cover most of the
property, with the volcanic flows
occurring as a strip across one end of
the property. Intruding into all these
rocks is a dyke swarm of quartz
monzonite porphyry.

During the last field season a
detailed geochemical survey was
carried out on the property. The
results of these samples were treated
statistically to distinguish between
the background samples and the
anomalous samples. The anomalous
copper and molybdenum areas were then
outlined. These areas were of three
types: high Mo-high Cu, high Mo-low Cu
and high Cu-low Mo.
Later in the summer a number of
soil profiles were taken across one of
each type of anomalous area. Using
atomic absorption, these samples were
analyzed for total Cu and total Mo. A
number of the samples were also
selected for partial analysis using
S.D.T.A., as an aid in distinguishing
between significant and non-significant
anomalous areas.
The copper and molybdenum values
for the entire property were treated
statistically to determine what effect
topography had on their distribution.
The results of treatment showed lower
mean and standard deviation values for
the hilltops than for the valley
bottoms. The values for the valley
slopes were intermediate between the
hilltops and the valley bottoms.

Taking into account the pH of the soil, the soil type, the underlying rock
type, the topographic location' and the copper and molybdenum distribution
revealed by the soil profiles, a criterion was formed to distinguish between
significant and non-significant anomalous areas.
38

�THE STRUCTURE, STRATIGRAPHY AND PETROLOGY OF THE
NORTH END OF THE ABITIBI BLOCK 7, STURGEON LAKE,
ONTARIO

Lou Covello
The Sturgeon Lake greenstone belt is typical of the rhyolite-andesite-basalt
assemblage of Archean metavolcanic rocks in the Canadian Shield.
It consists of thick
volcano-sedimentary pile, broadly symformal in morphology with a central outcropping of
infolded coarse, poorly sorted metasediments flanked to the north and south by the main
metavolcanic sequence. The entire greenstone belt is engulfed in a gneissic basement
complex and intruded by numerous late Archean granitic plutons.
The north end of Abitibi Block 7 comprises a sequence of felsic and intermediate
metavolcanics lying on the south side of the greenstone belt. Detailed mapping of this
area has revealed the lithology to have a uniform east-west strike and near vertical dip.
Individual rock units are essentially lens-like and relatively undeformed. Metamorphism
is of greenschist facies, the common mineral assemblage being quartz, albite, carbonate
± chlorite, ± epidote, ± muscovite, ± chloritoid.

Rhyolitic and rhyo-dacitic rocks tend to be pyroclastic in origin, while more
mafic members often occur as pillow lavas, or vesicular and massive flows with minor
pyroclastic and ash-flow type interbeds.
PAST EXPERIENCE:
2

summers with Ontario Department of Mines in Timmins and Sault Ste. Marie, Ontario.

2

summers with Anaconda out of the Lakehead.

1

winter with Planet Mining of Sydney, Australia in North Queensland and Victoria.

1

summer with Noranda Exploration in Northwestern Quebec.

1

year with Mattagami Lake Mines, Sturgeon Lake, Ontario.

39

�GENERAL STRATIGRAPHY AND TRACE ELEMENT DISTRIBUTION
OF THE SEDIMENTS OF BLACK BAY, LAKE SUPERIOR

R. D.

Middaugh

During the late summer of 1970 a reconnaisance survey of the bottom sediments of
Black Bay was carried out. The sampling was done from a Boston Whaler using a Phleger
gravity corer and a Ponar grab sampler. Unfortunately, due to weather conditions only
32 stations were completed.
Samples, on being brought to the laboratory underwent various analysis. Grain
size analysis were done using sieve and pipette methods. The Ph and Eh were recorded
at the top and at various depths along the length of the core.
The cores were split
and logged and samples were taken at various intervals of x-ray diffractometer analysis
and for trace element analysis using the Atomic Absorption unit.
The trace elements
analysed for were Cu, Fe, Mn, Cr, and Ni.

Results of the x-ray diffractometer analysis indicate that there are three units
present.
Glacially derived clay, 2) post glacial intermediate clay, 3) upper
1)
recent sediments. These units are conformable in the deeper parts of the bay but
exhibit erosional contacts near the more shallow margins.
The geochemical data indicate that the trace element concentrations are independent of grain size.
The data would also seem to indicate that the trace element
concentrations are fairly uniform and show no anomalous values either vertically or
horizontally relative to the lithology of the sediments of Black Bay.

EXPERIENCE

:

Summer 1968 - General mapping and core logging in the Papaskwasati Basin
and the Otish Mountains in North Central Quebec.

Spring 1969, 70, 71 - Limnological studies of Lake Superior under J.
Mothersill and Canada Centre for Inland Waters.

40

S.

�.

.

Experience: Ontario Department of Mines
Ontario Department of Mines
Projex Ltd. - 1970

-

I

-

196-9

968

AMPHIBOLES AND PYROXENES FROM THE SYENTITIC ROCKS
OF COLDWELL ALKALINE COMPLEX, THUNDER BAY, ONTARIO
M.

C.

Lee

Amphiboles and pyroxenes are separated from the rock specimens which are syenites
and nepheline syenites from the Coldwell Alakaline Complex.
The amphiboles and pyroxenes are determined by both optical and x-ray powder methods.

The 2V angles, extinction angles and refractive indexes (a,
3, y&gt;) are determined
for these specimens.
The pyroxenes are found to be soda augite, aegirine-augite and augite.
Zoning is observed; there is an enrichment in aegirine content towards the rim of the crystals.
The amphiboles determined by the optical studies are proved to be ferrohastingsite,
hastingsite, and also some riebeckite. Zoning is also observed; the iron content increases
from the center towards the rim of the crystals.

Optical determination is a much better method than that of x-ray for these minerals.
X-ray determination is a failure for the pyroxenes and amphiboles.
It is due to the fact that
the cell parameters of diposide is very similar to those of aegirine and augite.
The same
factor affects the x-ray determination of amphiboles; the cell parameters of riebeckite is
very similar to those of ferrohastingste and arfverdsonite
The course of crystallization of these pyroxenes seems to be:- soda augite -&gt;
aegirine-augite -&gt; Aegirine. According to Aoki (1954) as well as Yaki (1966), crystallization
in the mentioned trend takes place under low temperature and high oxygen partial pressure
conditions. When the crystallization trend is moving towards the aegirine-rich members,
the temperature is decreasing gradually and the oxygen partial pressure is increasing
simultaneously

From the analytical results; the sequence; - Ferrohastingsite - Arfvedsonite is
suspected to be continuous. Formerly, both riebeckite and arfredsonite are suspected to be
the final end product.
The presence of riebeckite in some rock specimens of Coldwell Complex
has shown that riebeckite is the final end member of the series.

41

�AilAA&gt;
COMPANY

• MULTINATIONAL MINING
• FACING

"If

TOMORROWS CHALLENGES
The mining industry faces serious challenges
in the coming decades in meeting its basic

youngfolkstoday are looking

CAREERS WITH A
CHALLENGE — with social

for

—-

responsibility
to their

RESPONSIBILITIES and

GATIONS

with service

—

fellowmen

itsOBLI-

fulfilling

to protect environmental values.

The very foundation of the standards that all
PEOPLE seek to achieve is based on a growing and adequate supply of MINERALS.

they

need not look further (than
the mining industry)."

K MacGregor
Chairman and Chief Executive Officer
American Metal Climax. Inc
I

AMAX

activities include the exploration,
development, mining, smelting, refining and

processing of nearly half the metals

in

the

periodic tables.

Group
IA

1

1

A

NIB

VB

IV.B

VIB

VlIB

IMA

IIB

IB

VIII

IVA

1

H
Hydrogen
00797

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3

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Li

m
6 939

11

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l
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4

5

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B

C

Beryllium
9 0122

Boron

CaAon

10 811

12 0i» '5

12

13

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2

Mg

Sodium

Magnesium

22 9898

24 312

;

14

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S.i.con
28 086
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19

1 20

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21

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1

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39 102

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Scandium

Calcium'
40 08

37

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38
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47 90

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40
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Rubidium

55

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56

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8

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l

132 905

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18
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51

41

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Niobium
92 906

57-71

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89

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1

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17849

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(227)

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Uranium

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EXPLORATION,

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93

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48

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If

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l

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29
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76

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2

94

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3

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II

22

Pluton-

9

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2

(242)

INC.

A SUBSIDIARY OF AMERICAN METAL CLIMAX, INC.

i

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190 2

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95

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(243)

2

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?

195 09

f

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24
9
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1

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96

97

Cm

IS

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25
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(245)

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-(249)

69

2

80

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18
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in

TORONTO, KIRKLAND LAKE, TIMMINS,
WINNIPEG, KAMLOOPS, VANCOUVER
42

��:

3 rd

::

YEAR

Patrick Fung
Interests:
Geochemistry

Experience
Ontario Department
of Mines - Mapping
Research Assistant
at Lakehead
University
t

Allan Chan
Interests'
Ore deposits

Experience:
Mapping, geophysics,
geochemistry, claim
staking with
Falconbridge Nickel
Mines, Ltd.

Ed Grootenboer
Interests:
Exploration Geology

Experience
Seven years employed
in all phases of
exploration geology

Brent Paske
Interests:
Structural Geology

Experience
2 years mapping with
the Ontario Department
of Mines

Joe Kasarda

Interests;
Mapping and Structural
Geology

Experience:
Ontario Department of
Mines 1969
Conwest Exploration
Co. Ltd. 1970

John F. Scott
Interests:
Mineralogy, Petrology

Experience
Varied, in North
Western Ontario

44

�::

:

::

2nd YEAR
George Einar son
Interests:
Geochemistry

Experience
Engineering surveys with the Department of Highways

Ron Green
Interests:
Economic Geology

Experience
Recent transfer from Chemical
Engineering - no field w oi k
in Geology as yet

Bob Kyryluk

Interests:
Geophysics, music

Experience:
Prospecting in British Columbia

Stuart McEwen

Interests
Exploration Geology

Experience
Griffith Mine, Red Lake — summers
of 1969-70
Rich Niels

Interests
Geological Mapping, Geology field trips. Photography,
Skiing, Fencing, Jude
I

Experience
Geological Mapping with the Ontario Department of
Mines - summers of 1 965—"70
45

�:

Allan Speed
Interests:
Passing Geology

Experience:
1917 - Gieat Lakes Nickel
l9bS - Great Lakes Nickel

Brian Nieminen
Interests:
Structural Geology

Experience:
2 summers at Ontario Water
Resources Commission Chem labs
- water testing
Les Tihor

Interests:
Prospecting, Photography

Experience:
1967 - Noranda Explorations
1908 - Falconbridge Nickel Mines
1969 - Noranda Explorations
1970 - Falconbridge Nickel Mines

Paul Strandberg
Interests:
Exploration Geophysics
and Petrology

Experience!
Ontario Department of
Mines Geophysical
Party - summer 1970
Juris Zdanovskis
Interests:
Prospecting, Hunting and fishing,
Photography
Experience:
Noranda Mines - summers of 1 966-69
Falconbridge - 1970

Gord Trimble
Interests:
Economic and Mineralogical Geologj

Experience
Worked with Falconbridge on recent New Brunswick
ore find - summer of 1970
46

��Mr. George Einarson, second year Geology Major student, has been awarded a
J.P. Bickell Foundation Scholarship valued at 1,500 dollars. This award is made on
the basis of five A grades in first year studies and is paid over a three year
period, providing a sufficient average is maintained. Mr. Einarson was born in
Winnipeg but moved to Thunder Bay in 1955 with his family. He attended Westgate
Collegiate and Churchill High Schools, and continued directly on to studies in the
Geology program at Lakehead University. He becomes the second student majoring in
Geology to receive a Bickell Scholarship. Mr. Patrick Fung, now a third year
student was awarded his scholarship in the Fall of 1969.

noranda
Noranda Exploration Company Limited
no personal

liability

Branch Office

253

Lincoln St.

Thunder Bay

48

�49

�You may never have a community named after you,
but you might make one happen.
The modern-day
given him three
hero. Today,
geologist.

it's

would have
called him
they call him

explorer. Years ago, they
ships, a Godspefed,

a helicopter.

Modern-day

And

explorer.

and

today,

And, possibly hero.

ment

of that

first

discovery. Inco can

munity happen. But Inco cannot do
Inco.

The

International Nickel

name for career. A

rewarding,

make
it

this

com-

without you.

Company. Another

fulfilling career.

It

could

one day he may set down his modern-day ship
upon a wilderness. And, on that day, he just may find
an ore body. And a community will be born. A com-

be yours. For further information on employment op-

munity with opportunity for developers, processors,

44,

For

designers and more. Opportunity that will be fulfilled

without

sacrificing the natural

beauty and environ-

portunities with Inco, please write the Supervisor of

Recruiting and Employment, International Nickel, Box

Toronto Dominion Centre, Toronto 111.
You may never have a community named
but you might make one happen.

INTERNATIONAL NICKEL
THE INTERNATIONAL NICKEL COMPANY OF CANADA, LIMITED

ADS-2-71
iCOCKFIELD,

1-4565

BROWN &amp; COMPANY

LIMITED /TORONTO

50

after

you,

��52

�.

ei&gt;4

Dr E. H.

Chown

Do vole University,

Montreal
Topic: "The Geology of the Otish Mountains,
Central Quebec".

Dr J. Tuzo Wilson
Principal of Erindale College and Professor of Geophysics at the University
of Toronto
Topic: "Continental Drift and Plate
Tectonics"

Dr E. Irving
Earth Physics Branch
Department of Energy, Mines and Resources
Topic: " The Origin of Marine Magnetic
Anomalies"

Dr M. M. Kehlenbeck
Queen's University
As of July 1st, 1971, Assistant Professor of Geology, Lakehead University
Topic: "Deformation and Recrystallization Textures in the Pipmuacan
Anorthosite, Quebec".

Patrick W. G. Brock
Visiting Professor, Queen's College of City
University of New York
Topic: "Precambrian Shield in East Africa: structural
age relationships of intrusive and metesomatic
alkaline rocks.
Geomorphological studies of Fast
African Rift Valleys".

53

�Dr, R. H. Ridler, Ph.D.

,

University of Wisconsin

Two years post-doctoral study, University of Western
Ontario,

Presently, Research Scientist, Geological Survey of
Canada,
Five summers with the Ontario Department of Mines,

Research

Archaean volcanic stratigraphy and mettallogeny, in
particular exhalite and gold.

Gold Metallogeny and the Geological Cycle in the Archaean Abstract

Archaean geology is characterized by polycyclic assemblages of related plutonic, volcanic and
sedimentary rocks representing the de-sialification of the proto-mantle. The ideal cycle
comprises, from oldest to youngest, a mafic volcanic plate accompanied by mafic intrusives; a
felsic volcanic pile accompanied by felsic intrusives; and annuli of volcanigenic sediments.
Folding may precede or follow a cycle or, rarely, intervene between members of a cycle. Regional
deformation and metamorphism conclude the Archaean; stabilization, uplift and brittle failure
follow.

Intrusive, volcanic and sedimentary phases of a cycle have accompanying syngenetic gold mineralization.
Both clastic and chemical sedimentary deposits are known. Volcanigenic chemical
sediments (exhalites) are particularly favourable.

Exhalites have traditionally been classified into oxide, carbonate, sulfide and silicate facies
to which arsenide, sulfate, and halide should be added. A further subdivision into sub facies based
on cation population is proposed, e.g. (Fe/Cu/Zn/Ag/Pb/(Au?)
sulfide. Sampling of diverse
)
species of exhalite at the south margin of the Abitibi Basin indicates a close affinity of gold
and sulfur.
Ductile and brittle deformation and metamorphism have recrystallized and remobilized the gold
anomalies to varying degrees. Complex gold-quartz vein histories are a common result but
migration of gold is restricted to a few tens of feet or less.

CLIFFS

CANADA

OF
Active

Mine

Exploration and

Management

Property

204

in

LIMITED

in

Submissions

Canada
Invited

Toronto - Dominion Bank
Thunder Bay , Ontario

54

Bldg.

�O'*
We

are interested

in

receiving submissions
on properties of merit
for

examination and

possible

option

in

Canada or elsewhere

SUITE 1309-7 KING STREET EAST

TORONTO

I,

CANADA
55

LIMITED

�Report on First Year Field Trips

by
Eric Brown and Dave Powers

Under the supervision of Dr. Mercy, Dr. Mothersill and Dr. Franklin, we first year Geology
students proceeded on two field excursions. The first involved a three-fold purpose: one, to
acquaint us with the unconformable nature of the Sibley Archean contact, and the paraconformable
nature of the Sibley-Rove contact; two, to observe bedding, ripple marks, a sedimentary sequence
of chert, mudstone, sandstone and conglomerate; three, to view some diabase sheets which cut
across the bedding. On the second field trip we proceeded to Pardee Township and Pigeon River to
observe cuestas, dykes and concretions in the Rove shale. This trip also took us to the exploratory site of Great Lakes Nickel Company.
Our first stop on the Sibley group field trip was at the site of the Wolf River. Here the professors pointed out to us the sequence of varved clays in the sedimentary bedding through which the
Wolf River has cut. The next stop, at a gravel pit near Kama Bay hill, served somewhat the same
purpose - to illustrate the bedding and distribution of grain sizes. At Kama Hill a number of
geomorphological features were pointed out to us. They included the following: a large anticlinal
fold; interbedded mudstone and sandstone;
small lenticular or discontinuous diabase sills; a
chert horizon, with fine lamination of interbedded carbonate and anthraxolite
massive mudstone;
purple shale; and a thick diabase cap rock.
;

After these observations we moved on to scrutinize a deposit of red sedimentary rocks that had been
intruded by a diabase sill. This sill had penetrated down through the sedimentary rocks into the
Archean basement. We made our next stop in the region around Red Rock, and saw several outcrops
of Sibley rocks, followed by a region of granite outcrops.
The next point of interest was a
quarry composed of black Rove shale overlying a Gunflint formation. Embedded within the Rove
shale were large, irregular carbonate concretions, possibly of organic origin.
The final stop of
this trip brought us to an exposed basal unit of the Sibley group which is comprised of polymictic
conglomerates. Here also was exhibited a well-defined contact zone between the conglomerate and
sandstone.

On the second field trip we headed south to the United States border. A range of eroded mountains
known as the "Norwesters", which includes Mount MacKay, follows the east side of the highway. The
cuestas are composed of black shale (Rove formation) with a diabase cap. As we proceeded southward,
the topography changed to one of more rugged relief which is related to the bedrock geological
changes.
The Great Lakes Nickel Company exploration project was the first stop on this trip. Our group
climbed up to the adit, which was constructed by the company into the sulphide zone, to investigate
the rocks in and near the adit. After stripping the adit of most of the available chalcopyrite
outcrops, we returned to the bus. On our next stop at the Middle Falls Campground on the Pigeon
River, we were mainly concerned with the diabase dyke which cut across the region and gave rise to
the falls. The dyke crossed the highway to where it cut into a Rove shale formation; the contact
zone between the dyke and the shale was closely observed. Also, the same carbonate mineral
concretions evident at the Rove shale quarry mentioned before were evident here.

Our last stop was at the end of Memory Lookout Road. At the lookout it was pointed out that we
were standing on a dyke which could be visually followed (intermittently) to the south, as it
stands up above the surrounding country rock in that area. Two other dykes could also be observed
which ran parallel to the dyke on which we were standing.
The significance of these field trips was not fully realized until such time in the academic year
when some of the processes involved in the formation of these geomorphological features were
comprehended.

56

��Report on Field Trip to Study Soifie Features
of the Coldwell Alkali Complex
1

Sept. Sth-llth, 1970
by Pat Fung

Party: Director: Dr. H. Loubat
Members: 3rd year students, Lakehead University
A. Chan, P. Fung, J. Kasarda, B. Paske, J. Scott

Our field trip was intended to study some interesting features of tte
Coldwell Alkali complex. The main stops we made, together with a general
geological map of the area, are given in the map below.

This complex was intruded into the Archean Greenstone belt in Keeweenawan time (+1065 m.y. to
1225 m.y.). At stop 4 the gabbro of the complex comes into gradual contact with the impure arkose
of the Greenstone belt, forming a contact metamorphic aureole of gneiss. At some places lenses and
veins of quartz, aplite and calcite, with pockets of syenite were found in the gabbro; and in some
outcrops, magmatic bandings in the gabbro were seen.
These features indicate an intrusion of a
mainly gabbroic magma with local varieties and perhaps a later intrusion of syenite. The contact
at stop 9 was much simpler. Walking east we passed from highly metamorphosed (granulite facies?)
we ll-bedded claystone, through lenses and veinlets of syenite which increased in content until,
through a few tens of metres, it was pure syenite.

58

�For exIn several outcrops we saw xenoiiths of different sizes and composition, mainly basalt.
ample, at stop 2, just off the highway, was a large xenolith of basalt, and at stops 3 and 4 there
were xenoiiths of basalt and breccia in the syenite. Most of them showed evidence of slow sinking.
F. Puskas suggested that these were from the Coubran Lake volcanic cap and that the intrusion was a
lopolith where the present level of exposure is near roof. The consistent fracture and shear zones
For instance, at stop 4 there was a domelike
might also expose some interesting structures.
structure with pre-Coldwell rock sheared and fractured on top of the Coldwell gabbro. Also, at
stop 9 near the western margin of the complex, there were two main directions of fracture - one
vertical and one horizontal in the south-east direction.
The rocks in the complex show complicated structural and age relationships as well as diversified
composition.
The oldest was the gabbro, followed by laurvakite, syenite and related rocks. But
at stop 4, within a few feet the gabbro changed in composition from common to leucocratic gabbro due
This change might be due to the interaction of syenite with
to an increase in acidic content.
gabbro (hybridisation).
The laurvakite also shows variations in composition - at stop 1 it was
much altered, with plenty of quartz, calcite and pegmatite veins. The laurvakite is also rich in
olivine in molybdenite, and native Mo., but in areas such as stop 8 it is very fresh and approaches
In stops
the composition of a syenite. Most impressive of all are the variations in the syenite.
At stop 2
2 and 8, the feldspars are very pinkish, probably rich in hematite due to alteration.
it was intruded by the rhombopyre dyke near the Bamoos Radio Station, implying an older age
relative to the rhombopyre dyke. At these stops, the syenite shows an intersertal texture of the
potassium feldspars in a matrix of mainly mafic minerals, with evidence of agpaiitic sequence of
crystallization.
The syenite is much altered whereas the rhombopyre is rather fresh.

At stop 4 we actually saw some xenoiiths of syenite in the gabbro, but at stop 5 the nephelene
was very prevalent in the syenite, which is rather fresh with alteration only of nephelene to
zeolite.
Finally at stop 5 » on our way down the railway road near Port Coldwell, we saw the fresh
nephelene syenite dying out into the altered, pinkish normal type of syenite - and yet at stop 7
two series of syenite veins cut each other, in diabase.
These observations imply that the
intrusion is not as simple as F. Puskas has anticipated. It can only be explained by the occurrence of multi-stage crystallization and local variation in the order of crystallization.
Generally, the main part of gabbro crystallized out first, then the normal syenite which became
altered either before or during the intrusion of the rhombopyre dyke, followed by the intrusion of
the syenite by the dyke.
A second and significant portion of syenite rich in nephelene crystallized
out, breaking up some older syenite and the rhombopyre dyke.
Somewhere another, but insignificant,
portion of gabbro crystallized out and engulfed some of the older syenite.
The laurvakite generally fits into the pattern after the crystallization of the first portion of
gabbro, but another part might have formed later - or the change in composition and amount of
alteration can be attributed to local magmatic differentiation and environment alone.

Ae seen at stops 1 and 5» the pegmatites and others in various rock types were always of late
origin.
They usually occurred in veinlets of the parent rocks and showed similar mineralogy, but
their grain size and composition altered relative to the distance from contact.
For example, the
pegmatite at stop 6 can be attributed to the late magmatic portion of magma rich in volatiles,
crystallized in fractures in the already solid rock. Since the whole complex is generally rich in
rare minerals and elements, it might be interesting to do a chemical analysis of these pegmatites.
There are also some features of geochemical interest, one being the agpaiitic sequence of crystallization in the altered intersertal syenite. Another is the interaction among various rock types
To mention
evident in the xenoiiths and surrounding rocks, and the contact between various veins.
a few, the xenoiiths of gabbro in syenite (stop 7)» remained fresh and retained sharp boundaries;
the rhombopyres and breccia at the same stop showed similar features. But several hundred feet
away, the two series of syenite veins in the so-called nephelene syenite veins showed where they
cross-cut each other in a complete fusion of their contact.
This can be explained by the
similarities and differences in the composition of the host and foreign material. When syenite
veins meet and cut each other, it is not hard chemically for solution and recrystallization near
the contact, whereas the reaction between a gabbro and a syenite is much more difficult, if not
impossible.
The alteration in nephelene syenite to colourful zeolite might be worth studying too.

Mineralization occurred in several places. Common ores such as pyrrhotite, pyrite, chalcopyrite
and iron oxides were seen in many outcrops in small amounts. But at stop 1 the molybdenite
associated with laurvakite is rather rare. Further study might reveal yet other interesting
elements and minerals such as titanium. At stop 8 large amounts of magnetite were seen either in
nearly pure forms or injected into the surrounding rocks such as syenite and gabbro.

59

�Besides the rhombopyre dykes mentioned above, there are several dykes cutting the complex. At
stop 3 two vertical dykes cut the syenite. These and the one at stop 7 were diabasic and might
be related to the Keeweenawan extrusives in Central Canada. Also at stop 8 there were several
series of high angle dykes of olivine-basalt in various host rocks. These and other structures,
such as the sill of basalt at stop 6 might be the equivalent of Animekie extrusives, but further
study is necessary to substantiate this. One way to do this is by radiometric dating and the
initial 87Sn/86Sn ratio which should be the same for all co-magmatic rocks. These and other
studies might reveal the relationship of these structures to the other regional phenomena, such
as the dykes which might be feeders to the regional Keeweenawan extrusives.
The rocks in the complex itself are very interesting and spectacular in their variety, texture,
rare minerals and elements, and in the sequence of crystallization. Economically the potential of
nephelene syenite and laurvakite for construction material, and the other rare elements might be
worth investigating. Further study may contribute to the understanding of pre-Cambrian stratigraphy in the Canadian Shield or even in the crust.

Subsequent Field Trips
1 .

Sibley Penninsuia field trip

2.

Kakabeka Falls - Armstrong field trip

3.

Shebandowan field trip

4.

ShebandDwan undei ground field trip

60

�The
LongView
(Home, photographed from 22,000 miles away)

Most

of us at

Texas Gulf have

children. Many, including the

president, have young children.
These are a multitude of

reasons why the long view of
the world is a way of life at
Texas Gulf Sulphur Company.
Even without the children, a

company which has been
in developing natural
resources over several
generations would emphasize
long-range planning, thinking in
terms not just of five or ten
years ahead, but 20, 50 and 100
years. A major mine with its
processing and related facilities

successful

must be viable for at least two
decades rf it is to be rewarding
to stockholders, employees and
the community.

Executives of natural
resources companies learn to
contemplate the prospects for
developing natural resources
for their children

and

children’s

children; the materials for

continued growth in the developed regions of the earth; the
requirements for eradicating
poverty, disease and starvation
in less

privileged parts of the

globe and the wherewithal for

them on the way to fuller
development. They must think of
how these things may be done

setting

without disturbing man’s environment in unacceptable ways.
The long view is a way of life
for us.
Texas Gulf Sulphur Company.

������</text>
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                    <text>�Digitized by the Internet Archive
in

2015

https://archive.org/details/lugeologyjour1972

�LAKEHEAD UNIVERSITY

JOURNAL

GEOLOGY

SECOND
EDITION
1971

EDITOR

DAVE POWERS

-

72

CO -EDITOR
RON WRIGLEY

�Looking to the future
...

today.

Rio Algom
Rio Tinto
120 Adelaide Street West
Toronto

1,

Ontario

�'Dedicatum

It is cLi^tcuLt to know where to begin oh. to end a dedication to Trevor W.
There were ao many h acets o h kit, career that it is impoAAible to do justice
Page.
to alt oh them.

Khter graduation h.rom the University oh Idaho in 940, "Trev" enlisted in
the R.C.A.F. and impatiently waited h°r World War II to terminate ao he could return
to his iiut love - exploration.
He came back to mining afiter discharge and i&gt;et out
to gain oa much varied experience as poAAible oa a prelude to entering the academic
1

circle.

Though AometimeA unorthodox, "Trev" iA remembered by his AtudentA oa a
dedicated and AucceAA^ul diAAeminator o h practical knowledge.
He alwayA had an
example firom kiA perAonal experience to illuAtrate a point during lecturer or labA.
I n addition to kiA devotion to hard rock exploration,
"Trev" became very
interested in the Pleistocene oh Thunder Bay Vistrict. He made a detailed Atudy oh
the results o h local glaciation and at the time oh his death was completing the fairst
drafit oh a thesis on the Aubject requirement h°r a Master oh Science degree.

The dedication oh the year book to the memory oh T. W. Page, B .Sc., P.Eng.
is laudable.
The department oh Geology has developed hrom Aingle instructor AtatuA
to a major department within the Faculty oh Science.
It is appropriate that the
contribution made by that Aingle inAtructor Ahould be remembered and recorded.

M.

W.

Bartley, P.Eng.

�Once more the Geology Club of Lakehead University
has demonstrated considerable enterprise in publishing

this yearbook.

It seems to be a particular talent of

our students in the Department of Geology to become

thoroughly involved in the corporate interests of the
Department and, indeed, of the University as well.

Their

major contribution to the rescue of the last Carnival
Week from the soggy sands of pernicious neglect was one
of the best examples of healthy and constructive student

involvement in the affairs of this University that has
been apparent in the past year.

Currently, the University is examining the implications for its future development that are

contained in two public reports of the provincial government's Commission on Post-Secondary
Education.

One of these is in final form and refers only to the Northwestern Ontario region while

the other is concerned in its "draft edition" with all of Ontario.

Reactions to both briefs have

been mixed and provocative descriptions of their contents commonplace.

Certainly as the Universit-

ies consume so many of the dollars in the public purse there is no gainsaying the taxpayer's right
to expect accountability, but invoices or balance sheets do not quantify the short or long-term

value of a university education to the individual, and through him or her perhaps even to the body
corporate.

In the last analysis there can be no

substitute for the goals which are achieved by

individual effort and it is within our own compass to rise above misleading and often substandard

proposals set by dilettantes or opportunists.

Their ideas are passe in any event, unless history

lies and the boiling point of water is 5,000°K!

It is a pleasure to commend the students in the Faculty of Science and particularly those in

the Department of Geology for their past efforts in their studies and to wish all many happy and

successful years ahead in their studies and in their chosen professions.

I

am pleased to con-

gratulate all of the Geology students who have worked with care and vigour to produce this excellent
yearbook.

A. Ross,
(Dean, Faculty of Science).

R.

�The production oh this second volume oh the

Journal encourages

Geology

students oh our

me in my belieh that the

Department axe amongst the liveliest

in the University. Your co-operative ehhort expresses
an underlying interest in and concern hor oar commun-

ity o^ purpose

which Is to sustain

and

enlarge the

study and knowledge oh the earth sciences.

Everywhere in

Canada

there

is

a strong

upsurge oh enthusiasm hor the science oh geology and students are coming into the universities

in unprecedented numbers.

The demand hor highly

educated and qualihied prohessionals is sure

and steady and, even on the most pessimistic oh projections,
come.

The demand is not only hor geologists in the

will remain so

h 0&gt;

many years to

traditional areas oh petroleum and mining

geology but is also hor people specializing in hydrogeology , oceanography
ology and, a very new phenomenon, in High School teaching oh geology,

,

environmental ge-

khtex many years

oh

neglect the prohession in Canada is beginning to be recognized as an essential and vital part
oh our society.

you are learning how to become part oh that prohession so that you may join a group
oh Canadians

world.

The

whose work is known and

respected by their scientihic colleagues all over the

responsibility hor becoming

worthy members oh a great prohession rests on your

shoulders

Edward Mercy,
CHAIRMAN,
Geology Department.

Vr.

�with compliments

from
the faculty of
science

lakehead university

Dean

R. A.

Ross

�I

�e&gt;

'led-ct

d

LES TIHOR, President Geology Club

This has been by faor the busiest yean, yet faor the
Geology Club. But begone mentioning its activities I
would like to Introduce the executive faor the past year:

PRESIDENT
SECRETARY
TREASURER
YEARBOOK EV1T0R
SOCIAL DIRECTOR

-

-

Let Tihor
Beth Hillary
Eric Bn own
Vave Powers
Brenda Cooper

F ortunately

the club a faint t exploit ofa the yean, woa
what woa to faoZlow. The members decided
to AuppZement out meagre budget by AetZlng hunting mapA
dating mooAe A eat on.
But, due to poor weather conditio nA
and out late Atant, we sold only Alx mapA wonth eleven
doZZant and, we were threatened with a falfaty dollar falne
Afaten thlt dlsfaor erecting AlgnA on a Queen' A highway.
appolntlng experience, however, thlngA began working very
well Indeed.
no Indication

ofa

,

Morale woa very high In the geology department and
tkit wat evidenced by the tremendouA Aupport Ahown In club actlvitlet.
In the Eonettent' annual
canoe race, faor Instance, 35 percent ofa the students enrolled In geology participated [thlt Included
one Aneaky farogman'.
We didn’t win anything but It began to become obvious to the Atudent body
that there were geologists around.
)

The club again made ItA pretence known by ret cuing the annual Winter Carnival King and Queen
contett, previously cancelled due to Atudent apathy.
Amazingly, an activity that no one had teemed
to want anymore turned out to be a faantattlc tuccett.
During carnival week we alto ’acquired’ the
Engineer’ A prize cannon and actioned It ofafa to the highest bidder.
Thlt wat In retaliation faor
their kidnapping the geology Prlncett and holding her faor ransom. The $56. proceedt ofa this farlendly confaticl went to the CNIB.

Along more academic liner, the club members enjoyed an Interesting and Infaormative underground
tour ofa International Nickel’s new mine at Shebandowan, Ont. We very sincerely thank INCO and In
particular, Mr. J. Vance, Mine Geologist faor their time and co-operation, and faor a wonderfaul
dinner.

We were faortunate also to have a number ofa falne speakers farom various parts
A part ofa this book is dedicated to these speakers and their topics.

ofa

Canada and the

U.S.A.

Finally, In addition to a number ofa parties throughout the year, the Geology Club sponsored
L.U.’s Wind-Up Dance ofa the year.
The pro fails farom this dance provided the last crucial part ofa
the revenue needed to guarantee publication ofa this book.

All In all, it was a falne year faor the Geology Club and I would like to thank all those who
made It so. A special hand, goes to our Year Book Editor, Dave Powers, and his stafafa who have put
in a great many hours to make this second Yearbook a standard to be aimed at In the fauture years.

Les Tlhor.

�Following in the footsteps of last year's "Year Book"
the groundwork for the new edition in early Fall.

book is to make our presence known.

success we began

Our primary purpose for the year

And what better way to accomplish this than

to advertise our Department!

I

should like to take this time to thank each Professor and all the members

of the Geology Department for contributing to the success of our second Year Book.
A special thanks is extended to Mrs. Jean Helliwell, the Geology Secretary, whose

typing skills and business experience proved to be invaluable;

and to Mr. Sam

Spivak, the Geology draftsman, with his drafting and artistic talent in giving us
a hand by drafting the crests and advertisements.

The experience of working with this year's staff has been an enjoyable one,
and an experience

I

hope next year's second year class will take up and enjoy.

Thanks to my staff for their patience and time:

Ron Wrigley

Co -editor

Rob Larsen

Advertising Manager

Les Tihor
Bob Scott
Ron Green
Brian Tittley

Photographers

Gary Grabowski

Layout Manager

Eric Brown
Beth Hillary
Barry Pinn

Layout

Dave Powers,
Editor.

�Kakabeka

����V&gt;l.

John S. Mo£h&amp;u&gt;WL,

8. Sc. [Phyiich) {CanJL&amp;ton Univ.j;
Gzolog-ical Engi.ntzAJ.ng)
Quttn'A UnivzAAity)
[GtoZogy] (Quttn'-i UniveAAity)

8 .Sc.
Ph.V.

•

(

(

Background

Geologist

-

Standard Oil Company of New Jersey

Senior Geologist- Mobil International Oil Company,
Basin analysis in Nigeria, Colombia and Southern Africa

Associate Professor

-

Lakehead University

Reader - University of Nigeria, Nsukka, Nigeria
(Sabbatical leave 197 2/7 3)

Research
1)

Limnological studies of Lake Superior.

2)

Mesozoic stratigraphy of Western Canada.

3)

Limnological studies of Lakes Chad, Albert and
the Niger Delta.

Limnological studies of the Canadian portion of Lake Superior were carried out for
the third field season under contract to the Canada Centre for Inland Waters, Burlington, Ont.
To date nearly two-thirds of the Canadian portion of Lake Superior has been covered by a
regional survey grid. During the 1971 field season the studies provided employment opportunities
for the following students for at least part of the summer:
Patrick Fung, George Einarson,
Allan Speed, Beth Hillary, Peter Friske, Bob Kyryluk, Keith Heckley, Eric Brown and Dave Powers.
A survey of the lake-proper was carried out from the Martin Karlsen between Pigeon
River and Marathon along north-south lines every five minutes of longitude (approximately
four miles)
Benthos cores and Shipek grab samples of the lake-bottom sediments were taken
at 325 stations and an echo sounding survey was carried out between sampling stations.
In
addition 110 stations were sampled in Nipigon Bay along a grid, two minutes of longitude by
one minute of latitude (approximately 1.0 miles by 1.5 miles), from a Boston Whaler using a
Ponar grab sampler and Phleger corer.
.

The following information has been compiled into map form to show the distribution
of
1)

the Eh and pH measurements of the lake-bottom waters and sediments;

2)

the first map of the lake-bottom topography in nearly 50 years;

3)

the grain size and mineralogical distribution of the lake-bottom sediments;

4)

the amounts of organic carbon, total carbon, iron, manganese, nickel, copper,
zinc, chromium, strontium and mercury in the lake-bottom sediments.

5)

the Quaternary stratigraphy.

The regional limnological studies of the Canadian portion of Lake Superior will
probably be completed during the 1973 field season

�VR. HENRI LOUBAT, Geological Engineer,
A^iiitant PAofieAAOA, Lakehead
Pk.V. Geneva;

Llniveuity
Bold astonomers occasionally suggest a variation of
physical parameters such as the gravitation "constant",
since the birth of the solar system. But we don'.t have
to go so far in the hypotheses to reasonably assume that
if we are going back 3.10^ years, the earth's aspect
has been somewhat different from what it was in recent
geological times, during the last 600 m.y. for instance.
In these very old Archean times, the size, shape,
thickness of crustal (continental?) plates, the depth
and nature of the oceans, the atmosphere, the climates
were probably different from what they are now. Although
some volcanic and sedimentary features seem similar to
recent phenomena, we can reasonably guess other rates
of volcanism and sedimentation, other relationships
between crust and mantle in these remote times.
If now we focus our interest on metamorphism, we could expect that the pattern of regional metamorphism has to be different in Archean and recent orogenies.
It is easy to understand that the
metamorphism of rocks is not only due to the absolute pressure and temperature, but also (and
mainly) to the rate of the physical actions, to the trends of those "stresses": if for example
the mass of crustal plates was much smaller than the mass of the recent continental plates, if
the heat flow (beside volatile activities, H 2 O, CC&gt; 2
and if the rate of sedimentation were
also different, the pattern and the definition of metamorphic facies would be different from the
classic schemes that we know from the works of Barrow, Turner, Winkler and others, working on
much less ancient orogenies.
.

. )

For instance, if the absence of glaucophane-schist facies is confirmed in Archean belts,
this could eventually indicate that narrow belts of extreme pressure and weak increase of
temperature were missing in these times, indicative of smaller, lighter colliding crustal
masses.

At the onset, with
It seems promising to initiate a systematic study along these trends.
the best thing to do would be to investigate several limited areas in "greenstone
belts" and to clarify what I call the "style" of metamorphism. We shall have, of course, to
discriminate what is to be attributed to the many thermal aureoles around magmatic intrusions,
also to discriminate the diaphthoresis from an initial 'positive' metamorphism.
a limited team,

Among many other fields, this one could confirm Thunder Bay as a major location for geological studies and research.

�VR. JAMES M. FRANKLIN, B.Sc. [CanJi^ton)
M.Sc.
CaAJteXon );
Ph.V. (MeAteAn)

;

(

AAA-iAtunt Pao^zaaoa.

MID-WEST SUPERIOR GEOTRAVERSE RESEARCH GROUP
During the first half of this century, many of the
world s prominent geologists maintained that Precambrian
Shields are composed predominantly of granite and contorted metamorphic gneiss.
The apparent complexity of the
geology was exemplified in those areas immediately
adjacent to the relatively simple Phanerozoic rocks of
the United States.
Unfortunately, Precambrian rocks of
New York and immediately north of the eastern States
belong to the Grenville Province, and area affected by
at least three orogenic periods.
The Grenville Province
is understandably structurally and petrologically complex.
Had these geologists ventured north to Noranda, Timmins or
Northwestern Ontario, they would have quickly realized
that some portions of the Shield are less structurally complex than the Appalachians, and that
distinct time and lithostratigraphic subdivision of the shield is possible.
'

In the past 20 years, application of standard stratigraphic, structural, and petrographic
techniques has resulted in unlocking the apparent secrets of the Precambrian. We now realize that
that the oldest (Archean) areas of the shield are composed of three major elements, the economically
important "greenstone" or volcanic belts, the metamorphosed and high deformed sedimentary or
"gneiss" belts, and an assortment of granitic and mafic intrusive rocks.
The first two "stratified"
elements show remarkable stratigraphic continuity. Perplexing problems remain however. What type
of "volcano" and volcanic structure was present during Archean time? Are the greenstone belts
precursors to our present day "island arc" belts? On what type of crust were these volcanos built
and what representatives of the ancient primeval crust do we see today? What mechanism has
deformed the belts relatively intensively, yet metamorphosed them so little? What is the origin of
the sedimentary detritus, and why are the sedimentary deposits highly metamorphosed and deformed,
relative to the volanic areas? How old are the Archean rocks, and what tectonic stages are
represented by these sequences?

These and many other interesting problems have gained the attention of many geologists, but
limited access, incomplete mapping, and the necessity of employing a divergence of specialists in
order to attack a problem, have prevented geologists from finding the answers. A group of 12
geologists have thus joined together as a result of a necessity of using "team approach" to solving
Archean mysteries, to form the Mid-west Superior Geotraverse Research Group.
The research group is directed by Dr. A. M. Goodwin of the University of Toronto and includes
Dr. Currie (U ot T) , Dr. Schwerdtner (U of T)
and Dr. Kehlenbeck (Lakehead) as a structural geology
team, Drs. Fawcett and Goodwin (U of T) and Dr. Loubat (Lakehead) as petrologists Drs West, Halls,
Farquhar and York (U of T - Geophysics) as geophysicists and geochronologists Dr. Mercy as geochemist, Dr. Naldrett (U of T) and myself as economic geologists. Dr. L. Ayres of the Ontario
Department of Mines and Dr. J. 0. Wheeler of the Geological Survey of Canada are acting as
Government liaison personnel. The group has taken as its area of study a broad "corridor" extending
north from Shebandowan to Pickle Lake. The corridor encompasses at least three volcanic belts and
,

,

.

,

It contains virtually an entire suite of Precambrian lithotypes and
The corridor is
traversed by several roads and railroads, and further access may be gained by the abundant lakes
and rivers of the area.

two sedimentary gneiss belts.

is probably completely representative of Canadian Shield Archean geology.

Several participants have initiated studies:
Currie is studying structure and paleomagnetism
near Lac des Mille Lacs.
Farquhar and York are applying the new Ar39/Ar40 techniques to dating
metamorphosed rocks. Halls is examining the application of paleomagnetic techniques to Archean
rocks.
Goodwin has initiated petrochemical studies in the English River gneiss belt. I have undertaken a study of the base metal deposits in the Sturgeon Lake area. This summer Dr. Loubat will
begin studies of metamorphic isogrades in Volcanic rocks, Dr. Kehlenbeck will study the structural
domains associated with sedimentary-intrusive sequences north of Thunder Bay.
The Geotraverse studies will probably continue for a period of ten years.
The ultimate
objective is to test several hypothetical "models" of Archean geology in order to find a more
suitable explanation for the observed features.

�V&gt;i.

Manned
M.S.

M.

K&amp;kZcnbcck,

[SytijOLc.uA

8. A.

c UvuvchA-ity)

(Hofafria.
;

Ph.V.

UniveAAiXy)
[Quccn'A Univ.)

Background
Research Associate for Adirondack Project Consulting
Geologist (Ground Water)

Geologist for Quebec Department of Natural Resources

Visiting Professor at University of New Brunswick
Assistant Professor,

Lakehead University

Research

Petrography and metamorphism of rocks in the Little
Moose Mountain syncline, Adirondack Mountains, New York.
Deformation textures in plutonic rocks, specifically
anorthosites.

My initiation into the geological problems of Precambrian terrains was in 1960 while
attending Syracuse University.
There, I was fortunate to participate in a research project which
was then just starting.
Our investigation focused on the south-central portion on the Adirondack
Mountains of New York. Simultaneously other universities were working on their research projects,
so that the entire Adirondacks were receiving renewed scrutiny from many disciplines of geology.
Of particular interest to me was the metamorphic petrology and structure of the Grenville
metasedimentary sequences. Among the results of the field work was the establishment of four subfacies within the granulite facies as well as a distinction between basement and supracrustal
rocks as defined by lithologic character, structure, and total rock textures.
In 1965 I left the Adirondacks, moved north across the Frontenac axis, and entered
into the Grenville Province proper.
During the next four years I became acquainted with the
geologic complexities of southeastern Ontario and Quebec.

My association with the Grenville Project provided me with an invaluable learning
experience.
This project undertaken by the Quebec Department of Natural Resources involves
4-mile reconnaissance mapping of areas bounded by two degrees longitude and two degrees
latitude (approximately 10,000 square miles) per field season. The value of such field work
lies in the vast amount of geological information which is gathered in a single summer.
To facilitate the analysis of the voluminous data, computer techniques were developed.
This enabled standardization of data input, providing consistency in the recorded observations
of all participating geologists.
Computer treatment of the geological data greatly increased
the time available for interpretation and extended the manipulations to which the data could be
subjected.

After nearly ten years of field experience with highly deformed and metamorphosed
Precambrian rocks, my interests have become more and more centered on the structural evolution
of Precambrian shield areas.
Reconstructions of evolutionary paths rely heavily upon recognition
of structural domains and on an understanding of their place in the tectonic framework.
This
is especially important if the absence of distinctive lithologies or structural trends prevents
clear delineation of major structures.

�An example is the Lac Rouvray anorthosite massif in Quebec.
Investigating textures
produced by cataclasis and recrystallization has shown that this igneous intrusion displays
a spectrum of whole-rock textures ranging from primary igneous to completely metamorphic
Hence the amount of deformation, in this case primarily recrystallization and cataclasis,
is variable from place to place and defines distinctive structural domains.
These deformation
textures demonstrate that this course-grained igneous rock was in places completely reworked
to a metamorphic gneiss bearing little resemblance to its ancestor, (Plate 1)
The
petrologic implications of this could be far reaching when considering the origin of the vast
monotonous "seas" of quartzof eldspathic gneisses so abundant in shield areas.
.

Since my arrival at Lakehead University last September I had had limited opportunity
to study the local geology; however, I hope to remedy this as soon as the snow melts.

Plate

1

Plagioclase-biotite gneiss derived from
anorthosite by complete recrystallization.

�Vn. M. W.

Sasitlny,

Spe&amp;lal LecXuAeA.
A GEOLOGIST
I was invited to contribute a personal experience to
this edition of the Year Book. What better example than
becoming a geologist.
It is unlikely that my experience
is greatly different from the majority of other graduates
in geology.

During my secondary school tenure I was exposed to
the usual humanities and sciences but do not recall any
reference to the solid earth science. On entering
University in 1930, I elected Science as a broad area of
study.
The curriculum required enrollment in four
sciences, english, a foreign language, and a non-science
elective. Not being biology oriented, I selected the
unknown, geology, to complement chemistry, physics and
mathematics.
The subject proved so interesting due
primarily to the enthusiasm of the professors and the
senior students that I was more than delighted with my selection. After four years of intensive
instruction in the basic phases of the discipline plus two summer seasons prospecting, I graduated.
Now I am a geologist - so I thought.
My application for summer employment with the Ontario Department of Mines as a field assistI was certain that
ant was accepted and I was assigned to a survey party as a junior assistant.
at the close of the field season I would be forced to choose from a variety of responsible
positions offered by government and industry. After all, I was a GEOLOGIST. No offers came.
After three months of waiting, I partially realized my naivity and went searching for a position.
The Provincial and Federal Departments were well staffed with men holding post-graduate
degrees and/or several years' experience. They would require junior assistants next field season.
My enquiries to exploration and mining companies envinced similar replies, but some did have jobs
(not positions) open as survey helpers and draughtsmen, underground samplers, mill and mine helpers
and university graduates would be favourably considered.
Not for me, I was a GEOLOGIST.

During my search for a position suitable to a B. Sc. in geology, I fortunately encountered a
senior consulting geologist who offered sage advice and thereby brought me back to reality. He
reminded me that I was only a graduate in geology, not a geologist. He convinced me that I might
become a geologist in five or ten years depending on how hard I worked at gaining experience and
increasing my knowledge. This came as quite a shock. He pointed out that although I had been
provided with a sound geological academic training, this was only the beginning.
I must now
augment this training with practical experience and if possible attain post-graduate degrees
concurrently.
In reply to my query as to how this might be achieved since there was no positions
commensurate to my academic accomplishments available, he delivered a never-to-be-forgotton lecture
The gist of the lecture was for me to descent from my lofty pedestal, realize that my degree was
only a tool, and seek a job in the industry which would further my general education. He went on
to explain that a geologist must have an appreciation and general knowledge of the associated arts
of exploration, mining, mineral dressing, and evaluation.
The logical methods of acquiring this
knowledge were to work as an assistant or helper in any category on an exploration project, in an
operating mine, and in a mine engineering office. Above all, to observe the work of others in
many different operations and endeavour to learn all I could about the other man's job in order
that I could have a fuller concept of solid earth science.
I followed his advice and worked progressively as a core grabber and logger on diamond drills,
as a surveyor's helper on surface and underground, as an underground sampler and assayer, and as a
mine planning assistant as well as geological mapping during and after my po^:-graduate studies.

Some seven years after graduating with a Bachelor of Science in Geology,
sufficient experience and knowledge to be a GEOLOGIST.

M. W. BARTLEY.

I

felt that

I

had

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�MR. R.

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8 EMMETT,

Principal Ttc.hnicA.an.

'The Ancient Craft of Lapidary'

Lapis

- a

stone.

Lapidary - a person engaged in gem stone fashioning for adornment.
In fact Stone Age men were the first lapidaries
in as much as they gathered bright coloured pebbles
and rubbed them with sand and other rock to wear down
the rough surfaces and in doing so produced a semipolish in turn improving the colour of the stone.

As time passed between the ancients and the old
Chinese and Egyptian civilizations, various methods
were improved, i.e. the wheel was invented and the
ability to mount a piece of bamboo as a type of lathe,
the invention of bronze and iron and along with these
marvels the endless trial and error of various sands and minerals as abrasives.
The ancient Chinese lapidary started to work rock crystal with quartz sand.
This was a very
slow arduous task. Then some craftsmen started using red sand (garnet) and found that this cut
faster and did not break down so readily also that the fine powders gave a good polish.
In fact
garnet was used for centuries by the Chinese jade workers.
As for the ancient Egyptians, I am sure they used similar abrasives because of the outstanding finish on some of the lapis-lazuli ornaments found in the tombs, not forgetting the gorgeous
floor tiles of semi-precious minerals.
I am, however, more familiar with the Chinese workmanship.

There is a story told of a caravan arriving at a well known Chinese lapidary centre with bits
of a brown mineral which was said to scratch even the hardest stone.
Some of this was eventually
broken and ground down in the garnet mill (a stone wheel turned by a mule, similar to an old corn
mill)
It was then found that this new brown minerals was indeed harder and at once became much
sought after.
It was, in fact Corundum - no doubt weathered out from a Pegmatite and just lying
around
.

Now to the tools used.
To cut the larger pieces of jade, rock crystal, turquoise, etc. the bown string type of saw
was used, the string being replaced by a strip or rough wire of bronze.
The general method was
to sit two of the younger sons of the head craftsman one on either side of the piece to be cut,
charge the wire with abrasive and get going with push and pull
Many moons later it was cut
through, these were the days of "Wat no clock".
If a slab was required, the work simply started
again. All abrasive, no matter how fine, was re-cycled and used again and again.
I mentioned
bamboo tubes. These were extensively used in the making of beads;
the method is very simple and
is used to the present day with modern materials.
As the bamboo is hard when dry and has a
tubular structure down its length, it makes an ideal material to hold abrasive.
The material is
roughly formed by rolling and grinding, then it is held against one end of the tube. The tube is
filled with wadding or leather and abrasive applied.
The tube was then turned, not in full
revolutions but half turns by means of a simple pedal. The stone was soon ground to a smooth
ball.
I have done this myself and it works very well. The finished ball is now drilled to make
a bead using a bow drill and a bronze wire bit.
.

Over the years lapidary tools improved and gems were better cut and polished but I do not
have space here to enlarge on this aspect.
However, I will describe the workshop where I watched
and old craftsman work and where as a very special favour I was allowed to try the hand operated
equipment.
It was situated in the main room of St. James Square, Edinburgh, originally occupied

�It contained what appeared to be an Adam fireplace, the
by some member of the aristocracy.
windows were begrimed and the floor was like a small quarry with bags of rough stones lying
about. Mr. Begbie, the lapidary had worked there as a boy with his grand-uncle Mr. Cameron
who was himself a lapidary and seal engraver and when Mr. Cameron died, Mr. Begbie carried
on the business. Mr. Begbie was 83 years old when he died some six years ago. His workshop
has returned to dust as the whole square has now been demolished.

The workroom was still equipped with the old hand driven lap, or to be more precise hand driven skive which is a vertical shaft with a square boss in the centre to fit the
square hole in the turntable (or lap) made of lead and the whole assembly turning between
centres belt driven by hand operated shaft running parallel to it.

As it is very difficult to cut a gemstone whilst holding it in the bare fingers, a painThis is called a 'dop stick' and is
ful procedure anyway, a very simple holder is used.
usually made from a hard wooden rod, similar to old knitting needles, the diameter of the rod
approximating the size of the gem to be fashioned. The rod is about 6" x 8" long and tapered
To the other end is fixed a blob of wax, bees wax and resin in the old days, more
at one end.
recently yellow leaf shellac. This 'blob' is warmed over a spirit flame and the rough stone
is likewise treated and then bedded securely into the wax, leaving free the first surface to
be ground and polished.
When this side has been completed, the wax is warmed once again, the
stone removed and turned to the next surface and so on until the work is completed.
In order to grind a regular pattern of facets a 'Jab peg' is used.
This is a piece of
wood shaped like a small inverted gourd, 4V high, 2h" in diameter, tapering to 2" at the
bottom, a hole is drilled down through the centre so that it will fit on a vertical post at
the side of the lap.
The surface of the "Jab peg" has an arrangement of shallow holes
spiralling from the top to the bottom (see illustration)
The vertical post mentioned above
is situated about 2" from the edge of the lap and the "Jab peg" is secured to this by means
of a long tapered wedge.
Adjustment is obtained by raising or lowering the "Jab peg" on
the post and driving in the wedge.
The angle of the facet to be cut is obtained by placing
the tapered end of the 'dop stick' into the holes on the "Jab peg" and raising or lowering
the "Jab peg"
.

The abrasive used by Mr. Begbie was 'Emery' - a form of corundum with magnetite or
hematite - or what might be termed 'Bort' corundum. This powder is commercially ground
and sold in 1 lb. bags.
Each grade or grit of abrasive is stored in separate stone jars similar to the old type preserve jars - and each has a separate brush used to brush the
abrasive on to the lap. This lap is made of lead.
Lead you may ask is a strange metal to
use for a lap because it is soft as compared with other metals, but lead hardens with use
and becomes impregnated with the sharp abrasive.
This surface is very helpful when working
small fine facets.
The final polish of the gem is done on a block "Tin lap" using "rotten
stone" as the polishing agent.

Although this machine is hand-driven it is very accurate and relatively quiet and restful.
The results obtained are very satisfying.
However Patience is a virtue,
Possess it, if you can,
It's never in a woman.

And seldom

found in man,

and
If at first you don't succeed,

Try, try, try again.

The "Song of the Lapidary")

�SAMUEL T. SP1VAK
Vaa&amp;ting TectwA.cu.an
The Department of Geology has a fairly extensive map library comprising of approximately 3400 geolog-

ical maps,

including excellent coverage of Ontario

and

good coverage of the rest of Canada (Ontario Department
of Mines;

Geological Survey of Canada and Provincial

mapping agencies)

,

as well as partial map coverage of

the remaining countries (full coverage of Australia)

and the moon.
All Canadian maps are catalogued according to

publishers' series and cross indexed with the National

Topographic System.

Maps exclusive of Canada are catalogued according to the Library of Congress

classification and these methods enable anyone to go to our map library and immediately pick out
any map of a given area.

Geological maps are also catalogued according to approximately 96

different geological, geophysical, geomorphological , structural, physical, stratigraphic, economic
features so that if one wishes to, in a lecture, emphasize a specific geological aspect such as
faulting, folding, glacial features, etc., he is able to immediately pick out a map that best

illustrates this.

All the above information is stored on computer tapes and a print out of all

catalogues is readily obtained.

Drafting time is largely devoted to preparing drawings, overlays and maps for use by the

geology professors as teaching aids as well as catering to individual drafting needs which include
such projects as "Limnological Studies of Lake Superior" by Dr. J. S. Mothersill and (this year)
a

detailed field guide book to be used in conjunction with the 24th International Geological

Congress conference in August of 1972 (this section being organized by Dr. J. M. Franklin)

Throughout the year a considerable amount of drafting time is utilized by other departments in the Faculty of Science for the preparation of graphs, charts, sketches to be used in

published papers.
Two particular interests of this drafting department include:
a

i)

a project to prepare

geological relief model of the area from Marathon west to Atikokan and as far north as Armstrong.

I 'm

sure that this would give a better impression as to the relationship between geology and

topography in this particular area;

ii)

a more extensive and uniform rock-type legend system that

would allow a maximum flexibility by all geologists and cartographers.

S. T. Spivak

�For the past five years I have been employed by Dr J. S. Mothersill
in carrying out the research studies of Lake Superior supported by the National
Research Council of Canada and the Canada Centre for Inland Waters.
.

During the summer months I am required to prepare field equipment for
student assistants carrying out research studies along the lake shore and also
prepare supplies and equipment used for the major research vessel operations on
Lake Superior.
On the research vessel I am required to take a portion of the grab
sample for benthic fauna samples. The sample was thoroughly washed to remove
the clay and silt fraction.
The remaining sample was treated with magnesium
sulphate in order to separate the fauna from the remaining debris. The fauna
present in each sample were then placed in an alchohol-f illed vial for
preservation until identification could be made.

After the compilation of data from the lake the samples were brought
back to the lab for extensive study.

Representative cuts of approximately 100 grams weight were made from
each of the sand samples using the quarter ing-by-hand method. The grain-size
distribution of the sand fraction was determined at 0.25 phi(&lt;J&gt;)
intervals
using sieving methods, and the grain-size distribution of the remaining silt
and clay fraction was determined at 1.00 phi(&lt;f&gt;) intervals of pipette methods.
Cuts of the silt and clay samples were made from the core for grain-size
distribution which was determined at 1.00 phi(&lt;}&gt;) intervals by sieving and
pipette methods. After the grain-size analysis of these samples were calculated,
the figures were transferred on IBM sheets in order to determine the skewness,
kurtosis, standard deviation and mean size by computer.
Heavy mineral separations were carried out on representative sand
samples using tetrabromoethane (S.G.=2.94)
The heavy minerals were then
separated into magnetic susceptibility suites using a hand magnet and a Franz
magnetic separator at settings of 0.35, 0.80, 1.20 amps., and the non-magnetics
at 1.20 amps.
.

From cuts of the silt and clay samples from the cores I prepare
samples for x-ray diffractometry analysis along the sample preparation for
atomic absorption analysis.
After all the lab work has been completed, the data compiled and
the results calculated, I am required to type up all Dr. Mothersill 's papers
and reports, core description sheets, etc.

Pat Zurkan

�AWN

SUMPTER

T zc.hnA.CA.dn

There are sixty comprehensive sets of the more

important minerals, rocks and fossils from which the
first year Geology student learns the basic rules and

exceptions of identification and classification of

geological specimens.

These minerals, rocks and fossils are catalogued
into their specific groupings in such a way as to follow

exactly the general geology laboratory manual which was

composed by Dr. J. Mothersill of Lakehead University's
Geology Department.

With the aid of the manual and the specimens the first year student receives a good basis for
further geological studies.

Many of the specimens can be found locally as the students discover

when taken on field trips, and as a result, the student can associate specimens found in the
field with the specimens supplied in the laboratory by performing the same simple tests for ident-

ification, e.g.

oratory

hardness, cleavage, etc., as they use for identif icating specimens in the lab-

.

From the fossils the student learns how the age of sedimentary rocks are determined.

Following this the student learns basic structural geology such as stratification, layering
and foliation;
erosion;

then geomorphology which is the study of the changes in the landscape due to

culminating in the study of geological maps that show patterns of rock type outcrops,

stratas, faults and folds in fact all the information the student has learned in his or her first

year geology.

CONGRATULATIONS AND
to the

M. W. BARTLEY

BEST WISHES

Graduates

&amp;

ASSOCIATES

Geologists
202

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Bay, Ontario

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�MR. RICHARD L. STEPHENS

Szismic

Tzc.hnicA.oin

The Seismic Station at Lakehead University

began operation in March 1969 and is one in a network
of 28 stations in daily operation across Canada.

This

seismic network has been established in such a manner
that no point in the country is more than 300 miles from
a seismic station.

Recordings produced by these stations make
possible the detection and location of all major earthquakes, underground blasts, and nuclear explosions any-

where in the world.

Seismic records are produced by a

photographic process and must be changed and developed every 24 hours, along with the calibration
of recording and detection equipment.

Daily records are then annotated, analyzed and forwarded

to the Seismology Division of the Earth Physics Branch, EMR, Ottawa.

All major disturbances

recorded by stations are immediately telexed to Ottawa to permit rapid determination of precise

locations of events.

Seismic studies are based on measurements of the time at which a particular disturbance
was recorded, and the amount of ground motion it produced.

Seismologists are currently using

seismic records for such research projects as the determination of seismic risk zones in Canada;
the related problems of practical standards for earthquake-resistant construction; and invest-

igations of the regional properties of the earth's crust, mantle, and deep interior.

R.

L.

Stephens

�MR. VON MURRAY

GcochmiAtny Labonatony Technician
The geology research lab is located in Room CB 0021

with an auxilliary crushing lab in Room CB 0004.
The lab is equipped to handle most types of geo-

chemical analyses.

In addition to the chemicals, glass

and platinum ware, balances and furnaces necessary for

classical gravimetric analyses, the lab also has a Bausch
and Lomb Precision Colourimeter and a Perkin-Elmer Model
303 Atomic Absorption Spectrophotometer.

The latter two

instruments offer a rapid, precise method for major and
trace element analyses

Most first, second and third year geology majors will not have come in contact with the lab
as it is used only for research purposes by faculty and fourth year students.

This year Pat Fung

and Allan Chan have made extensive use of the lab while doing research for their thesis-seminar
course.

It is part of my responsibility to offer guidance and assistance to students using the

lab for these projects.
In addition to helping Pat and Allan

I

have done analyses for 1^0+ and f^O- on rock samples

for Dr. E. Mercy and trace element analysis by Atomic Absorption for Cu, Ni, Cr, Sr, Mn, Zn and Fe

on sediment samples for Dr. J. Mothersill.

My congratulations to the Geology Club for having a very active and successful year.

Don Murray,
Hon. B Sc
.

.

(Chem

. )

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��ALLAN chan. Fourth Year Honors

ELEMENT DISSEMINATION IN VOLCANIC ROCKS

Due to the variation in mineralogical composition
a suite of volcanic rocks should have a variation in

densities.

This variation may be a good indicator of

the different rock types.

Titanium, Potassium, Copper,

Zinc and Nickel are commonly found in rocks and may

give a basic indication of rock types.

With this in

mind the purpose of my thesis was:
1)

To find a simple analytical method of determining

rock types, especially distinguishing rhyolite from
rhyodacite, and andesite from basalt;
2)

similar to the major elements and;

3)

To see if the trace elements reflected a variation

To see if there is any significant trace element differ-

ence existing between the suite of volcanic rocks from Sturgeon Lake, a base metal area, and
Wawa, an area barren of base metals, which might indicate the presence of a massive sulphide

deposit.
In order to accomplish this the concentrations of K, Ti, Ni, Zn and Cu in sixty samples

were determined by using atomic absorption techniques.

Through experimentation it was found that the specific gravity method of classifying
volcanic rocks fails to give satisfactory results, but perhaps this is due to experimental error.
It is apparent that Zn is best correlated to TiC&gt;2 and K 0 and gives the best range of values
2

in the classification of volcanic rocks.

more or less not correlated in K 2 0 or Ti0 2

Cu is correlated better in TiC^/K^O only.
.

Allan Chan

And Ni is

�PATRICK FUNG

-

Fourth Year Honors

THE DISTRIBUTION OF IRON, MANGANESE AND TRACE
ELEMENTS IN THE WATER-SEDIMENT INTERFACE OF
CENTRAL NIPIGON BAY, LAKE SUPERIOR
The main topographic features of central Nipigon
Bay consist of a narrow, steep-sided channel; a shelfarea of variable width, being much wider along the north
shore than along the south shore and a shelf -break which
is predominant in the northern part and almost absent
in the southern part of the topographic channel.

The Eh and pH values on the water-sediment interface
samples indicate a slightly oxidizing and weakly alkaline
environment
There are three types of sediments found on the
lake-bottom: (1) a thin layer of sand occurring mainly
along the shores, (2) a sequence of Holocene siltclay sediments covering most of the topographic lows
and (3) a sequence of highly calcic Pleistocene varved
clays of variable thickness occurring mainly in topographic highs.
This sequence of sediments
under ly the other two types by erosional contacts.
The mineralogical composition of these sediments consists mainly of quartz, calcite, feldspars,
dolomite, illite, kaolinite, amphiboles and smectite-vermiculite interbeddings.
The quartz peak
is always the highest but the calcite peak in the varved sediments and the amphiboles and feldspars peaks in the silt-clay sediments reach considerable height.
The other peaks are always minor.
The areal distribution of the elements iron, manganese, nickel, copper, zinc, chromium and
strontium is affected by both the lithology and water-depth and on this basis, these elements can
be divided into four groups
Manganese
(1) The iron-group, including iron, copper, zinc and chromium
(3) Nickel
(2)
(4) Strontium

Relative to average sedimentary rocks, central Nipigon Bay is enriched in manganese, zinc
and copper and is depleted in strontium, nickel, iron and chromium.
Relative to the surface
sediments of Lake Superior, it is depleted in manganese, copper, nickel, zinc and chromium but
is enriched in strontium.
Relative to the top interval sediments of southern Lake Michigan,
it is enriched in chromium, copper, nickel, iron and manganese but is depleted in zinc.
Relative
to the surface sediments of the Pacific, it is depleted in iron, manganese, nickel and copper.

Strontium is probably camouflaged by calcium in the precipitated carbonates and is hence
enriched in the highly calcic varved sediments.
The differences in distribution between manganese and the iron-group of elements is attributed
mainly to the difference in stability of their ions and the different rates of post-depositional
dissolution and subsequent migration of these ions upwards along solution channels during
compaction.

The behaviour of nickel may be due to its affinity to the iron-group of elements on one hand
and to manganese on the other

Other factors affecting the distribution pattern may be the different amount of detrital
dilution due to different rates of sediment accumulation and to the different concentrations of
these elements in Lake Superior.

Fatriok Fung

�Modern mining exploration requires more
than a pick and a pan
Cominco

offers world markets an increasingly diversified product
range which requires the successful development of new sources
of metals and industrial minerals. Extensive and aggressive
is required to meet future needs and replace the ore
which Cominco is currently mining at approximately seven million
tons each year. To accomplish this Cominco spends several

exploration

million dollars annually

in

exploration programs

in

Canada, the

United States and overseas.

EMplopabion^oiMioo

CAMPBELL RED LAKE MINES LIMITED
BALMERTOWN, ONTARIO

EXPLORATION DIRECTED BY

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(CANA da) LIMITED

360 BAY STREET

TORONTO, ONTAR O
I

��THIRD YEAM
Neil Campling
Interests

Paleoenvironmentoloqy
Experience:
3 Seasons on Archeaological Digs

George Einarson
Interests
Petrology and Geochemistry
Experience
Summer 1971 - Limnogeoloqical reconnaissance of Lake
Superior under Or. J. Mothersill

Ron Green
Interests
Economic Geology

Tom Hong

Interests
Environmental Geology
Experience
Lands and Forests

Gob Kyryluk

Interests
Geophysics and Music
Experience
Prospecting in Gritish Columbia

�Howard Poulsen
Interests
Mining Geophysics and Exploration Geolony
Experience
6 years Exploration Geophysics
1 year EJA Ltd

Allan Speed

Interests

Geophysics
Experi ence
2

summers with Great Lakes Elickel Mines

1

summer with Dr. 3 . Mothersill doing

Limnogeclogical reconnaissance of Lake Superior

Leslie

A.

l'ihor

Interests

Photography
Experience
1

year with Goranda Explorations

3

years with Falconbridge Mines

1

year with the Geological Survey of Canada

Gord Trimble

Interests

Economic Geolooy

Experience
2

years with Falconbridge
3WK

�SECWOT WE/IM
Mike Andrews
Interests
Economic Geology
Experience
Summer 1971 - Ontario Department of Mines

Eric W. Brown
Interests
Structural Geolooy, Computer Programming
Experience
Summer 1971 - National Museums of Canada (Wawa)

Ralph Bullouah
Interests
Economic Geology
Experience
Summer 1971 - Ontario Department of Mines

David J. Busch
Interests
Geophysics
Experience
Diamond Drilling

Peter Friske
Interests
Geochemistry, Skiing, Tennis
Experience
Summer 1971 - Llmnogeological reconnaissance
of Lake Superior under Dr. J. Mothersill

�Gary P. B. Grabouski
Interests
Gptical mineralogy, Water-skiing

Bryan L. Heppler
Interests
Skiing, Skydiving, Environmental Geology

Beth Hillary

Interests
Geology Field Work, Oceanography, Petrology
Experience
Summer 1971 - Limnogeological reconnaissance
of Lake Superior under Dr. J. Mothersill

Dennis Kuiatkowski
Interests
Judo, Hunting, Fishing

Robert Larsen
Interests
Scuba Diving, Petrology, Skiing, Squash

Bernard Meyer
Interests

Experience
3 Seasons as Junior Assistant
uiith

0.

D.

M.

t

�Paul Nielsen
Interests
Economic Geology
Experience
Summer 1971 - Exploration with Matt-gami
Lake Mines

David Powers
Interests
Paleontology, Petrology, Photography
Experience
5ummer 1971 - National Museums of
Canada (Wawa)
- Limnogeoloqical survey
of Lake Superior under
Dr. J. Mothersill

Sharon Tihor
Interests
Leslie Tihor, Volcanology,
Geology in General

Ron (0. J.) Llrigley
Interests
Varied - Mostly Shipwrecks

I

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1st

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Michael

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Street East

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Steers, District Geologist

Room 204, 231 Arthur
(807) 345-2519

St.

LTD.

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Races

�Boy those sure are neat rock pictures

Strike, dip, lineetion, strike, dip,
lineation, strike, dip, lineation,
strike, dip, lineation, strike, dip,
lineation, strike, dip....

it.
Well if nothing else we could fish from

Now lad that isn't the way to
do it at all!

���every EN&amp;itVEER
Goo O GEOLOGIST

Qehvno

A

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�Intersection of the henoran and Hudsanian
cleavages

�Alex brown
Department of Geoloqical engineering
Ecole Poly technique Montreal
"
The White Pine Copper Deposit, hichiqan

Dr.

,

Dr.

H. V. UARREIM

University of British Columbia
"
Chat Canada's Piinino Industry Heans To
Canadians"

Mr.

BYRUIM

RICHARDS

A.B.P.G. Distinguished Lecturer 1971
"

The Beaver River Anticline And Its
Associated Giant Gas Reserves"

1

�GEOLOGY 71-72

aos

a
o
—

:—
zoukoco

zulu

�c $Announcements

�The GEOLOGY CLUB MouZd tike to extend their appreciation
to the

allowing people who*e contribution* throughout the court, e

oi the year, Mere instrumental to the Aucce** o&amp; both the Geology
"

Year Book" and the Geology Club.

Dr. M.

Kehlenbeck

ProfieAAor Lakehead University

Dr. R. Gregg

Proves* or Queen 'a UniverAlty

Mr*. Jean Heltlwell

Secretary, Geology Department

Mr. Sam Splvak

Draftsman, Geology Department

Ml** Cookie Polrer

Geology Prince*

Ml** Brenda Cooper

Social Director

M Iaa Su*an Turnbull

Student

Mi** Sandy Duncan

Student

M Iaa Brenda Duncan

Student

Ml** Lorna Nleml

Student

Mr.

Larry Ovifirichuk

Mr. G. Ha*hlgulcki

and to all member*

otf

Artist
Biology Photographic Technician

the Geology Department too numerous to mention.

�J

BONGARD

,

LESLIE

a

Co. LTD.

204 ARTHUR ST.
THUNDER BAY (P) ONT.

—

BONDS
MUTUAL FUNDS
— MGR.
BARON
S MALINOSKI — REP
SCHUSTER — REP.
TELEPHONE 344-6618
STOCKS
D.F.

F.

�GEOLOGY FIRST YEAR F1ELV TRIP
This year, the first year geology students had two opportunities to visit local areas of
geological interest. In most instances the sites we visited were natural occuring examples of
what we would be presented with in the geomorphological portion of the course this year.
Accompanying us on the trips were Dr. Mercy, Dr. Mother sill, Dr. Franklin, and Dr. Kehlenbeck
The purposes of the trips were to give us an over all
as well as several upper year students.
general idea of the geology of the area around Thunder Bay, which proved valuable to students
from southern Ontario as well as to examine some specific examples of bedding, dikes and unconformities
Our first stop on the Sibley group field trip was at the site of the Wolf River.
Here Dr.
Mothersill and Dr. Franklin pointed out the sequences of varved clays in the sedimentary bedding
through which the Wolf River has cut. Our next stop was at the Enterprise Mine. Here we saw
lead, zinc and silver ores.
We also saw sandstone beds underlaid by Precambrian rock, a difference of 1.9 billion years between the two rocks. The group was then taken to Pass Lake on
Sibley Peninsula. This brought us to an exposed basal unit of the Sibley Group which is comprised
of polymictic and conglomerates. We saw, also, a well-defined contrast zone between the conglomerates and sandstone. The last point of interest was a quarry composed of black Rove shale overlying a Gunflint Formation. Embedded within the Rove shale were large irregular carbonate
concretions, possibly of organic origin.
The second trip on October second, despite the rainy weather was participated in by about
thirty students.
The first stop of the day was at the spillway of the Kakebeka Falls Hydro
Station.
Because of the excavation it produced the best exposure of Gunflint tuff-argillite in
the area.
Here we noted a fault with strike parallel to the face of the spillway cut. This
site afforded an excellent opportunity to students who wished to collect samples as the area was
abundant in pyrite nodules embedded in the chert as well as pyrite veins. Areas of shale, limestone, tuff, greywacke and chert beds were also closely observed.
Close examination also revealed
anthroxolite in veins.
Our next stop at the Falls proper revealed a resistant chert-limestone cap which protected
the underlying shales from erosion due to the Falls.
Approximately one-half mile upstream from
the Falls we examined the point of contact between the Gunflint Formation and the older granite.
Next we proceeded to the point at which the Whitefish River crossed the road. A short
distance down stream we examined a unconformity between older granodiorite (igneous intrusive
rock) containing plagioclase and amphibole, and the Gunflint Formation.
At this point chert
mounds overlying the very thin basal conglomerate were observed. The chert mounds were believed
formed from very primitive algae
Proceeding south we came to the Pigeon River Middle Falls area. Here a gabbro dike in Black
Rove shale has produced an obstruction at right angles to the river movement which is resistant
to water erosion resulting in the Falls.
These black shale formations contained carbonate minerals
believed to be of organic origin 1.65 x 10l0 years old. Proceeding back to Thunder Bay we passed
through the range of eroded mountains called the "Norwesters" of which Mount McKay is an example.
These mountains are formed of black shale of the Rove Formation and are capped by a diabase layer
about 200 feet thick. The diabase which is resistant to erosion prevents the shale from being
eroded, reducing the mountains to a vertual peneplain.
As the year proceeded, we were better able to comprehend the forces which produced and are
destroying these features which we examined. We could also better comprehend these features as
they naturally occurred, which were set out rather idealistically in the course proper.
.

,

Barry Pinn,
First Year Geology Student.

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��GEOLOGY

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(1971)

��Canada

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                    <text>GEOLOGY
'73-'74

�1972 ·73·74

Lakehead University
UNIVERS~TY
DEPARTMENT .O F GEOLOGY

LAKEHEAD

THIRD

IDIIION

�Dr. A. D. Booth

�M. W. Bartley &amp;Associates limited
-

Geologists -

202 TORONTO- DOMINION BANK BLDG.
THUNDER BAY, ONTARIO

�1:

with compliments
from
the faculty of
•

sc1ence
lakehead university

Dean R. A. Ross

�Some readers of this Yearbook may know that
Lakehead University has recently been developing an Academic
Plan.
The first draft of this, usually called "The Skeleton"
because of its front cover adornment, sets out certain principles which I believe to be appropriate in the development of
this institution as a regional university.
Looking at Northwestern Ontario, a number of
points become obvious:
first, the possession of large tracts
of forest; second, the Canadian Shield and its relatively
unexplored geological wealth; third, the lake; and fourth, but
by no means the least important, the people of the region.

Lakehead already has a Forestry School of some
distinction and one which, we believe, in due course, should
be the best in Canada.
The Second of my primary areas of development is
Geology, and I can see that this is likely to expand in two
distinct phases.
In the first of these, the Exploration Geology
of Northwestern Ontario should be the object of the main thrust.
Certainly there is need for the discovery of new ore bodies.
Places such as Atikokan are dependent on existing resources, the
end of which is already in sight.
If new and important resources
can be found, particularly in that area, a pleasant town may be
saved from going the way of similar places in Alberta and British
Columbia which have become ghost towns.
This exploration phase,
which is important, both to regional economy and to pure geology
since it contributes, of course, to the theories of crustal
structure, will be followed and probably parallelled at some
point by what I can describe as Exploitation Geology which leads
indirectly to Mining Engineering.
The importance of the two
phases of the plan lies in the fact that industrial and commercial
backing for the university's activities should be forthcoming
and that the government will be ensured of the regional devotion
of our institution.
Another advantage of the plan, which involves
the participation of industry, lies in the employment possibilities
for students during vacations - something which is at the root of
instruction in all professional subjects.
I hope that these remarks may do something to inspire
the students in the Department of Geology with the importance of
their subject, their mission and their departments in the present
and future of this University.

ANDREW D. BOOTH

�MESSAGE FROM THE
DEAN OF SCIENCE

The principal problem facing Lakehead University this
year has been the decrease in student numbers .

This phenomenon

has occurred in practically all universities in North America and
Western Europe .

Lakehead has not endured a unique experience.

Perhaps a.n enrollment decrease would be regarded as a positive
factor if it could be interpreted as showing a trend towards a
higher quality and more dedicated studentry.

However, our fin -

ancial returns from the Provincial government are directly related to student numbers and when these decline significantly, the
institution trembles , becomes hypertensive and narrowly misses
the trauma of a corporate nervous collapse .
Such experiences occur regularly in industry and commerce.

If a commodity has lost favour in the market , then its

producers must revamp or replace it .

Failure to react success-

fully to this challenge generally results in personnel cutbacks
and plant closures .

Whereas the industrial environment is pre-

pared for such eventualities , the university one is not.

By

their very nature the universities attract staff of a highly
intellectual and sensitive type .

They are not well paid by

industrial standards , but forego pecuniary ambitions in favou r

�of a modest living which allows them the privilege of imparting
knowledge to their students and pursuing their own individual
research and scholarly work.

It is no criticism to state that

university professors and lecturers are less able to cope with
the rough, tumble and consequences of shifts in market-demand
than are their industrial counterparts. The fact is, however,
that they are becoming increasingly compelled to react to these
shifts.
Since the middle ages, all of the major institutions
of state and church in Western civilization have had to undergo
radical changes.
withered.

Some have survived the experience while others

The universities have endured minor perturbations

over these centuries, but have probably never been subjected to
the same external scrutiny as they are at present.

We all have

a responsibility to assuage and convince our critics through our
performances and actions of the tremendous and benevolent effect
that the university can and does have on our society.

We need

to have effective ambassadors, and, in the Faculty of Science at
Lakehead University, the Geology students are among the best
that we have. It is pleasure to be associated with them.
Once again, I am delighted to commend the enterprising
and good-humoured students in the Department of Geology for the
format and the high standard of the articles chosen for the
Geology Year Book.
Warmest congratulations and best wishes to all,

R. A. Ross,
(Dean, Faculty of Science).

�Union Miniere lxploratiuns and Mining corporation limited
A Subsidiary of

EXPLORATION
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~~~~&amp;
Geology Club of Lakehead University

~

The Exploration and Project Development Dept.

The Algoma Steel
Corporation, Limited
SAULT

STE . MARIE , ONTARIO .

�Dr. Edward Mercy

c

H A I R MA N

I

s

M E S S A G E

The publication of this, the third Year Book, demonstrates a
continuing involvement in their professional development by its
student contributors and organizers.

I am more than glad, on

behalf of the Department, to welcome this account of student
affairs during the past academic year.
The tradition of the Year Book is an excellent one and I
sincerely hope that , through your efforts , you will have established
the tradition in this Department so that those corning after you will
continue this good work.

There is no doubt that the Year Book makes

a significant contribution to the healthy growth of the Department.
To all who have helped in the production of this volume, my
heartiest congratulations.

Edward Mercy ,
Chairman .

�GRADUATE TO FALCONBRIDGI
Geologists, Geophysicists , Geochemists, Mineralogists
Mining and Electronic Technologists

FALCONBRIDGE NICKEL MINES LIMITED
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BALMERTOWN , ONTARIO

EXPLORATION DIRECTED BY

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SUITE 702 , 360 BAY STREET
TORONTO , ONTARIO

�PRESIDENT'S MESSAGE
This has been a very successful year for the Geology Club .
In keeping with the reputation we built for ourselves last year,
the Club took on the major role of the University's Winter
Carnival.

This was done by sponsoring the Queen and King contest.

Our two entries, Sharon Tihor and Doug Lehto faired very well.
Doug went on to be crowned Carnival King and will unfortunately
have to relinquish his throne next year, hopefully to another
Geology student.
Apart from Winter Carnival the Club put on two exceptionally
successful beer bashes.

As the academic year drew to a close the

Geology Club Social held in the Prosvita Hall marked the end of
the social calendar.
I would like to at this time to introduce the Executive of
the Geology Club for the past year, and to thank them for their
participation and dedication.
Vice-President:

Bob Scott

Secretary/Treasurer Eric Brown
Social Directors:

Ralph Bullough &amp; Peter Friske

Year Book Editor:

Barry Pinn

Special mention goes to Barry Pinn, Editor of the Geology
Year Book , and his staff for the laborious hours which they have
spent in the publication of an outstanding Year Book .

David Powers,
PRESIDENT,
GEOLOGY CLUB.

�ON THE GENESIS OF GRANITE
by
M.

YUMA

In the beginning God created the Heaven .•..•••.••....
and the Earth .
And the earth was without form , and void ; so begins a
well known story expounding a certain belief on the origin of
the earth and granite since granite is a rock occurring near
and on the surface of the earth . To a person supporting the
democratic principle, that the majority opinion is correct ,
this would explain the origin of granite satisfactorily . However, we, being individualistic and schooled in geology like to
think that this creation is not quite finished yet.
It must be admitted though that the origin of the
positive and negative changes that combine to form matter is
unknown . We, geologists, come into this when the earth was
without form , a swirling mass of dust and gasses, and imagine
that the ''force" of gravity was present which formed this
"ready created" dust into our earth .
It is assumed that the reader agrees that the earth
is a better sphere than the best basketball made by man; and
also that energetic (heated) matter tends to rise to the "surface", i.e. heat energy flows from a hotter to a conler object .
As a direct result of this remarkable observation , it
can be stated that the concentratio n of radioactive isotopes is
greatest in the rocks of the crust . Recall geothermal gradient .
Also it is known that the radiogenic heat output was greater
yesterday than today. Recall exponential decay function of all
radioactive elements. This would also imply that the surface
temperature of the earth, especially of granitic areas , was
higher in the distant past . This is shown by the gaseous envelope around it (all expelled from the earth) . Also water molecules cover 75 % of the surface .
Our "granite" stands out from the water , as the continental "floats". Recall isostasy . These continental " floats"
are essentially granites and their derivatives. They were and
are formed by contamination of the insoluble residue (silicon
dioxide and aluminum silicates) by the liquid remaining from
fractional crystallization of the basaltic magmas . This silica
enrichment must precede granite formation . This enrichment
occurs on the surface essentially . The contamination takes
place near the surface under cover of the very "wet'' sediments .
Bec~use of the lower density inherent in these "granitoid" rocks
and because of the badly fractured platy nature of the earth ' s
crust, these granitoid rocks tend to drift to the points of
highest gravitional field strength, which are presently in the

--

--

�vicinity of the poles. Guess where we find most of the earth's
granites? That's right , near the poles !
This is normal and expected since the earth is not a
perfect sphere .
The granites make up only about 1/ 10 of one percent of
the atoms in the earth but these are mighty important atoms for
us air breathing creatures .

SHERRITT

SHERRITT GORDON MINES LIMITED
MINING AND

MILLING

Lynn Lake , Manitoba

Personnel

DIVISION

PETER A. CAIN

Office

Vice President
Mining

( 204 ) 356-2441

�FIELD

�TRIPS

�1972-73

��SfPW«J

�Soetat

�Bi II Mclelland

Bruce Hicks

Frank Smit

Bill Blattner

Dave Evans

John Biczok

�Marvin Humphreys

Jeffrey Armstrong

William Eismont

James Rybar

John Carlin

First Year
1972.73

�NEIL R.

CAMPLING

Some Mineralogical, Textural and Environmental Aspects of the Pre-Gunflint &amp; Pre-Sibley Weathered
Profiles
In the Thunder Bay region, ancient weathered profiles
occur in the stratigraphic column below the initial sediments
of the Gunflint and Sibley Formations.
Both profiles consists of weathered granitic rock and a lithified, granitic
derivative.
The Pre-Gunflint profile is characterized by a remarkable increase in chlorite mineralization, and a very poorlydeveloped residual soil
texture.
These and other mineral ogical features tentatively indicate the Pre-Gunflint weathering occurred sub-aqueously in a temperature, estuarine
or tidal-flat environment.
The Pre-Sibley profile is characterised by an increase
in hematite mineralisation, and a well-developed residual
soil texture.
These and other mineralogical features
tentatively indicate that Pre-Sibley weathering occurred sub aerially in a humid, temperate climate.
Only the Pre-Sibley
weathered profile can be termed a paleosol .

�Pillow lavas from Archean volcanic-rich supracrustal units
the Superior Province of Northwestern Ontario were studied
on a regional scale to identify possible variations in the
style of metamorphism.
Chemical analyses indicate that metamorphism has not affected the basic chemistry of the pillow lavas in most cases.
Volatile contents vary in the lower grade of metamorphism,
however, significant metasomatism has occurred in only a few
localities.
Both tholeiitic and calc-alkaline chemical affinities were noted in pillows from various areas.
Chemical
variations within individual pillows which have undergone
relatively little alteration suggest differentiation processes
may have occurred during the crystallization of the pillows.
The pillow lavas of the Lake Nipigon-Geraldton-Jackfish
area are of a low metamorphic grade with mineral assemblages
corresponding to the greenschist facies.
Variations in the
scale of mineralogical homogeneity and the degre8 of recrystallization indicate that moderate pressure conditions prevailed
in the Highway 11 area between Beardmore and Longlac while
the Highway 17 area along the north shore of Lake Superior was
characterized by very low stress conditions.
This indicates a
variation in the regional metamorphic pattern with greater
depths of burial occurring in the northern volcanic-rich unit.
The regional metamorphic pattern in the southern volcanic-rich
unit may have been overprinted by thermal contact aureoles
related to intrusive plutons.
The suite of pill lavas from between the Highway 599 area
represents central amphibolite zones bounded to the north at
Central
Patricia and to the south of Sturgeon Lake by low
grade greenschist zones.
Mineralogical and textural evidence
suggests progressive regional metamorphism.

�THE GEOLOGY AND GEOCHEMISTRY OF THE ONAMAN LAKE
PROPERTY, NORTHWESTERN ONTARIO
In the thesis a detailed study was made of a small
mineral prospect. The Onaman Lake property is located
approximately 3 miles west of Onaman Lake in the Thunder
Bay Mining.Division. The property is underlain by five
rock types of Precambrian age: Keewatin acidic and mafic
volcanics, Temiskaming conglomerate. Algoman granite and
Keweenawan diabase dikes which cut all other rock types.
The intrusion of the Algoman granite has had a contact
metamorphic effect on the Keewatin mafic volcanics which
is characterized by the progressive development of actinolite-tremolite and epidote group minerals in an originally chlorite rich rock.
Cu, Zn and Pb are present on the property disseminated in quartz veins.
In order to study the possibility of discovering other occurrences of Cu and Zn, the
results of a soil sampling survey were evaluated statistically after separating the sample results into four
groups: organic Cu and Zn values and inorganic Cu and
Zn values. This study indicates a correlation between
geochemical results and observed mineralization but indicates very few other anomalous conditions on the property.

�STRUCTURES IN MIGMATIC ROCKS
For this study an area along the Spruce River Road was
chosen. Numerous outcrops in a 6 mile section were examined,
which a variety of structures occur.
Based on data, a three-fold division in the migmatite
complex has been made.
Well foliated biotite-plagioclase gneisses interlayered
with quartzo-feldspathic gneisses.
Lit-par-lit gneisses, composed of foliated gneisses
interlayered with a potassium feldspar-rich mobilizate.
Massive gneisses composed of poorly foliated rocks
with vague structures.
No sharp boundaries appear between these three types. A
some-what transitional relationship between structures and
mineralogy suggest stages in the degree of mobilization.
A complex tectonic history is demonstrated by the structures in the migmatite. These migmatitic rocks comprise a
basement complex overlain by less deformed and less metamorphosed metasedimentary and metavolcanic sequences. In the
migmatite complex a fluctuating temperature produced great
variations in the amount of melt at any time and thereby
affected the complexities observed in the structures.

�Archean Evolution of Western Dorion Twp. Ont.
The western part of Dorion Twp. shows evidence of Archean
ocks dating from very ancient 'primitive' basaltic crust to
late kinematic, quartz monzonites.
The oldest rocks underlie the northern part of the map area
consists of metamorphic rocks of predominan~ly sedimentary
nd, to a very minor extent, igneous origin.
These metasedients are represented by roof pendants and xenoliths of fine
medium grained, more or less plastically deformed, quartzoelspathic gneisses.
The metamorphosed igneous rocks exist as
ngular blocks of mafic to ultramafic hornblende gneiss.
The
atter may represent remnants of very early dykes, 'primitive'
saltic crust or possibly 'horses' of mantle material.
These
oof pendants and xenoliths float in a 'sea' of pegmatitic
o micropegmatitic, intensely flow-folded and very leucocratic
obilizate.
At the onset of the Kenoran 'orogeny' this basement assemb age began buckling in low amplitude east-west trending folds.
s these folds developed, the synformal portion, now represnted in the southern part of the map area by the greenstone
elt began filling with basement-derived pelitic· sediments,
ntercalated in later stages with minor amounts of basaltic
sh .
With time the rate of deformation accelerated and the
ressures and temperature became sufficiently high to remoblize the more volatile components of the basement at relatvely shallow depth .
This caused intrusion of small eastest elongate quartz monzonitic bodies along zones of structral weakness at the edge of the greenstone belt and within
he basement complex.
These same pressure-temperature
onditions caused progressive metamorphism of the pelitic
ediments and retrogressive metamorphism of the basement
omplex to a common middle-amphibolite facies grade.

�ALLAN SPEED
The Investigation into the use of Gamm-Ray
Spectrometry as a possible geologic mapping
tool
The uses of the~mma-ray spectrometry as a geophysical
tool in mineral exploration are well documented (Mero, 1960).
However, few investigations into the feasibility of using
this remote sensing technique as a geologic mapping tool are
known.
Thus, the purpose of this study was:
1) to investigate local scale variations in radioelement
levels between different lithologic units.
2) to investigate the mineralogical composition of the
various lithologic units causing the different radioelement levels.
3) to investigate the statistical problems involved in
collecting and presenting data of this type, and
4) to investigate the possibility of using gamma-ray
spectroscopy as a physical method which provides
information from which geological conclusions can
be drawn.
Of the many radioactive isotopes that occur in rocks,
only radio-potassium and members of the uranium and thorium
series are important geologic sources of gamma-radiation .
Two major,N-S traverses through the Gorham Township area
crossed granitic batholithic intrusives, two types of
sed~mentary rocks , volcanic rocks, diabase and gabbro.
A portable gamma-ray scintillometer was used to measure
the relative radiation effects of the various rock types.
The initial count data was converted into more meaningful
results using statistical methods , computer techniques,
and geochemical analyses.
These showed a definite difference in radioelement content of the various rock types
measured.

�JOE KASARDA
The Alteration and Trace Element Content
of the Mattabi Footwall Zone
The Mattabi orebody is situated in the Sturgeon Lake area
of North western Ontario.
It exhibits many of the features
common to Cu - Zn massive sulphide deposits found throughout
the Canadian Shield .
Alteration characteristics of the footwall rocks were
studied by means of thin sections made from approximately
45 collected hand specimens.
The main alteration products
observed were sericite and carbonate .
Abundant chloritoid
and a relatively low chlorite content suggest that magnesium
metasomatism was not prevalent during ore formation .
No
simple zonal arrangement of the lateration minerals is
apparent.
A total of 89 samples from 8 drill cores obtained from
the footwall rocks were analyzed for Cu , Zn, Ni, Ag , Fe , Mn
and Co2 by atomic absorption techniques.
The frequency
distributions of the elements were studied in the form of
cumulative frequency curves.
All the elemen~appear to be
approximately lognormally distributed.
Background and
threshold levels were graphically estimated.

�'

A BIOGEOCHEMISTRY STUDY OF POPULUS TREMULOIDES
APPROACHING A LEAD-ZINC-BARITE DEPOSIT
The purpose of this study is to compare the variation of
concentration of the trace elements lead, zinc, copper, and
manganese in the various portions of Populus tremuloides with
specific physical variables of the plant, such as height, age,
and diameter, as well as with soil chemistry.
The elemental levels of zinc, lead, copper, and manganese
were measured in samples of soil, bark, old growth, new growth
and buds of Populus tremuloides, and bark, old growth, new
growth plus buds and needles for Pinus banksiana. Solutions of
these samples were analyzed by atomic absorption methods.
Lead is the only element which shows an anomalous concentration in the bark, new growth, old growth and buds of poplar.
Old growth and new growth of poplar are the best portions of
the tree to sample in order to detect the presence of a lead
anomoly. The elemental concentration of lead, zinc, manganese,
and copper in the plant organs sampled is affected by the
absolute age of the species. The concentration of these elements does not accumulate with age.
With the shallow soil profile, as occurs over the Sibley
Group, geochemical soil sampling is a better exploration
method for locating lead-zinc-barite deposits than a biogeochemical survey using Populus tremuloides as a sampling species

�THE GEOCHEMISTRY OF THE LYON LAKE-CLAW LAKE SULPHIDE
BEARING GRAPHITIC SHALE, STURGEON LAKE, ONTARIO
The Lyon Lake-Claw Lake sulphide bearing graphitic shale
is contained within a predominantly sedimentary sequence of
course to fine clastics with minor carbonate and mafic volcanic rock.
Sulphide mineralogy consists mainly of pyrite and pyrrhotite occuring as nodules, lensoid pods and narrow bands
conformable with bedding. Traces of chalcopyrite, sphalerite
and arsenopyrite are present as well.
Cu, Zn, Ni, Co, Mn and As were analysed in sulphides,
graphitic shale and wall rock. Results suggest: (1) Sulphides
contain higher contents of Cu, Zn, Co, Ni and As than graphitic
shale or wall rock and (2) Mn, Zn, Co and Ni content decreases
eastward along the formation in graphitic shale.
Analyses of a vertical section through the formation
suggests: (1) Cu, Zn, and Mn are enriched in the footwall rocks
as opposed to the hanging wall rocks, (2) Zn and As are concentrated in graphitic shale in comparison with hanging wall
rocks and (3) Co and Ni content is relatively uniform throughout the section.
Element ratios have been used to investigate the depositional environment of sulphides and host rock. Results show:
(1) Co:Ni ratios in sulphides and graphitic shale are consistent with other worker's data for a sedimentary origin and (2)
Mn:Fe ratios are suggestive of volcanic contribution to the
Nestern margin of the formation.
Carbon content in the graphitic shale varies from 1.60 12.06 %. X-ray studies indicate carbon is either present in an
amorphous form or below the detection limit of this technique.
X-ray studies indicate the pyrrhotite present is monoclinic possibly derived by metamorphism from pyrite.
Evidence suggests that the graphitic shale is derived in
a sedimentary basin in which there was volcanic activity at the
western margin. This was followed by large scale mafic
volcanism. Sulphides derived by sedimentary or diagenetic processes is likely, since there is no evidence for a direct
volcanic exhalative source.

�AMOCO CANADA PETROLEUM COMPANY LTD.

Mining Division
Mining Properties Optioned, Developed
EASTERN OFFICE

WESTERN OFFICE

Suite 2010
65 Queen St. W.
Toronto 1, Ontario
Telephone: (416) 364-3409

2160 Guiness Tower
1055 W . Hastings St.
Vancouver 1, B.C.
Telephone: (604) 683-2591

PATINO MINES (QUEBEC) LIMITED
Fourteenth FIoor, 7 Kin g St reet East
Toronto , Ontario

�STRUCTURE OF AN ARCHEAN SEDIMENTARY SEQUENCE WITHIN
THE QUETICO GNEISSIC BELT
The purpose was to suggest a structural model for the metasedimentary rocks (Archean sediments). On structural grounds
it appears reasonable to this area to assume that the metasedimentary sequence rests on a basement complex. The unconformity between these two appears to have been remobilized
during orogeny and hence is no longer intact.
Based on field observation of sedimentary structures several reversals of top directions were determined. These sediments are basically of graywacke composition. Low-grade
metamorphism and non penetrative deformation have left primary
sedimentary features intact.
A maximum thickness of 4,700 feet of sediments was established from the model. The folding is tight isoclinal and
slightly overturned, originating from a flexural slip and flow
mechanism.

THE SILICATE AND SULPHIDE PETROLOGY OF THE
KAWENE LAKE INTRUSION
silicate and sulphide petrology of the Kawene Lake
Intrusion was studied using a transmitted light microscope,
a reflected light microscope, a 4-axis universal stage microscope, point counting, chemical analysis and x-ray methods to
determine if this intrusion is a strataform pluton, or an
alpine type ultramafic. A tectonic environment is also investigated and an origin for the rocks and sulphides is suggested.
It is found that this intrusion is not a strataform
pluton, but is possibly an alpine type ultramafic lying somewhere in between the two suggested and meffibers, namely the
ophiolite suites of Newfoundland and the serpentinites of
Vermont.
It is also found that this intrusion was syntectonically placed in an Archean eugeosyncline, surrounded by
flysh-type deposits. It is suggested that both the sulphur
and metal, essential to form the sulphides, came from the
magma itself and not from the surrounding rocks or the sea
water.

�• Mining Exploration
and Development
• Properties Examined,
Optioned and Financed
Phelps Dodge Corporation of Canada Ltmtled
Suole 1106 - 55 Yonge 51, Toronto, Onl M 5E I J4 ( 4 16) 366 4674
Suooe 404 , 1112 Wul Pender 51 , Vancouver I , B C ( 604) 684 - 6588
Suol t 409-491 Porl ogt Avt, Wonn•Pt&lt;l R38 2E5, Monolobo (204) 775 - 8423
Fredenc:ton. N 8 • Val d'Or, 0~

/

noranda
NORANDA EXPLORATION COMPANY, LTD.
NO PERSONAL LIABILITY

BRANCH OFFICE . .. ..
253 LINCOLN STREET
THUNDER BAY, ONT.

�V1t. Ed.waJtd MeJtc.y
V1t. MeJtc.y Wa6 boJtn and Jtec.eived ~ ea!tly
educ.a.;t{.on in geology at :the ImpeJtia.t CoUege on
Applied Sc.ienc.e and Tec.hnology in London,
England wheJte he Jtec.eived a B.Sc.. and Ph.V. in
geoc.he.m&lt;..6bty. V!t. MeJtc.y Wa6 ai.ho a SenioJt
Lec.:twteJt at :the UniveJtJ.JUy o6 Edinbu.Jtgh,
Sc.o:tland. Th!tough :the ye..a/U}, V1t. MeJtc.y ha6
done JteoeaJtc.h on geoc.hemic.a.t J.J:tudieo o6 plu:tonic. and volc.anic. Jtoc.k. in Eu.Jtope a6 well. a6
J.J:tudieo on u.tbtama6ic. Jtoc.k..6 a6 modw o6 :the
manile o6 :the EaJt:th.

V!t. Man6Jted Keh.tenbec.k.
V1t. Keh.tenbec.k. £00..6 boJtn in Bltemen, GeJtmany and
c.ame :to N. AmeJtic.a 6oJt ~ univeJtJ.Ji:ty educ.ation.
He J.J:tudied 6oJt ~ B.Sc.. in Ho6.6:tlta UniveJtJ.Ji:ty in
New YoJtk.. Coming :to Canada, he Jtec.eived ~
Ph. V. in Geology at Queen' .6 UniveJtJ.Ji:ty in KingJ.J:ton wheJte. he ha6 done Jteo e.aJtc.h in :the GJtenviUe
PJtovinc.e. A6:teJt one ye.aJt at U.N.B. he c.ame :to
L. U. in 1977 and i-6 piteo enily doing !teo e.aJtc.h on
:tec.:tonic. evo.tu:tion o6 :the Altc.hean c.JtuJ.J:t.

�V~.

M. W.

Ba~~ley

Bo~n ~n W~nn~peg, Man~~oba , unde~­
g~adua~e wo~~ a~ U n~ve~~~~y on Man~~oba ,
po~~-g~adua~e wo~~ a~ U n~ve~~~~y on
To~on~o.
F~eld Pa~~y Leade~ no~ On~a~­
~o Vepa~~men~ on M~ne~ du~~ng po~~­
g~adua~e yea~~.
Sub~equen~ly, Ch~en
Geolog~~~ and P~oduc~~on Manage~ a~
S~eep Roc~ I~on M~ne~ L~m~~ed.
F~~~~
P~~ncipal La~ehead Techn~cal In~~~~u~e.
F~~~~ Cha~~man, Boa~d on Gove~no~~.
La~ehead Un~ve~~~~y.
Cu~~en~ly ~n
p~~va~e p~ac~~ce a~ con~ul~an~ ~pec~al­
~z~ng ~n ne~~ou~ m~ne~al explo~a~~on and
developmen~.
Spec~al Lec~u~e~ a~ La~e­
head Un~ve~~~~y ~ince 7977-72 ~e~~~on.

V~ .

John S. MotheMill

V~ . Mo~heMill Uk:t..6 bo~n ~n Otill.IAXL, OntaJUo.
He ~ecuved lvi.-6 B.Sc. (Phy~~~ , Mathemati~)
at CM!eton UMveMdy and ~ B.Sc. (Geolog~cal Eng~ne~ng) and Ph .V. at Queen ' ~
UMveMdy. Wo~~ed no~ Stand~d 0~ (N.J.)
and Mob~ !~~national 0~ Co . ~n TM~ey,
Nig~, Colomb~ and EMope .
Jo~ned the
Faculty on La~ehead UMveMdy ~n 7966 . He
hM been caMy~ng ou~ ~ ed~e~olog~cal
~tud~eh o6 La~e Sup~o~ .
V~ng ~ ~ab­
batical leave he ~ed out ~e~entolog­
~cal ~tud~~ o6 La~e~ V~~o~ and Chad and
~he N~g~ VeUa .

�Bo~n ~n

Nohth Bay , On~ . B. SQ . and M. SQ .
a;t Ca.JLte;ton UMvVl.-6dy. Ph .V. ~n MetaLe.oge.ny
a;t .the. UMvVl.-6dy o6 Wu.tMn On.tilio . While.
¢.tlldy~ng 6o~ my Ph. V., I ~ a ge.olog~.t w~h
.the. Ge.olog~Qat Su~ve.y o6 Canada . I have. be.e.n
a;t Lak.e.he.ad UMvVl.-6dy 6o!t 4 ye.a.JU and my
~Ue.aJtQh ~n.tMe.¢t6 Me. ~n P~e.Qamb~n StJta;t,{.gMphy on .the. ThundM Bay d~.ttzid and MMJ.:J~ve. Sulphide. Ve.po-6~ 1 1.&gt; Genu~ .

~ . Md.e.wa.ine. ~ bo~n ~n To~on.to and a.t.te.nde.d
UMVMI.&gt;~Y ~n F~e.de.MQ.ton.
He. ~e.Qeive.d h.i...-6
B. SQ . and M. SQ . ~n geology a;t .the. UMve.Mdy
o6 New ~n~.&gt;wic.k. . On.tilio Ve.pM.tme.n.t o6 Mil-teA
hM be.e.n ~ . Mc.I.e.wa.ine. 1 1.&gt; e.mployM 6oJt .the. pM.t
.tMe.e. ye.a.JU ~n ThundM Bay . He. ~ g~v~ng .the.
.t&gt;e.d~e.n.tology QOu/1..6e. while. v~. J . Mo.the.Mill
~

on

~.&gt;abbilic.at

leave.

�V~. Roge.~ M~ehett

Bo~n -i..n FM-6R.e.y Yo~k6We. Eng.f.and , attended
ManehM t~ Un-i..veM~Ij wh~'l.e. he. ~eeuved M6
B. Se . and M. Se . de.g~e.M . Com-i..ng to Canada,
V~ . M~eheil 6tud-i..e.d 6o~ h-i..6 Ph. V. -i..n -i..6 atope. ge.oehe.rn.W~y at Mc.MMteJt Un-i..veM~Ij -i..n
Hamilion . S-i..nee. Mc.MMt~ he hM .6tu.d-i..e.d at
the. Un-i..ve.M~Ij o6 Af.beJtta and Un-i..veMUy o6
06R.o -i..n Noroway be.6o~e. eom-i..ng to Lakehead
Un-i..ve.M~Ij th-i..6 ye.~ .
V~ . M~eheil hM done.
~Me.~eh on .6u..f.phM -i.6otope..6, IU.mb~M
and ~Me eMth g e.oehem-i.6~y .

V~ .

H. Lou.bat

v~ . Lou.bat WM bo~n -i..n Sou.-i..aae. -i..n Sou.th~n
F~nee. .
He. ~e.euve.d h-i..6 e.~y edu.eation -i..n
Be.R.g-i..u.m and hanee. be.6o~e. eMolling at· the.
Uni.veM~Ij o6 Geneva -i..n SwUzeJt.e.and . Th~e.
he. 6tu.d-i..e.d 6o~ a B. Se . , M. Se . and Ph .V. -i..n
geoeogy and m-i..n~ogy M w~.e. M a d-i..p.f.oma
-i..n ge.o.f.og-i..ea.f. eng-i..ne.~ng . In EMope. he. had
done. wo~k p)()_nupaUy -i..n the. F~eneh and Ita.f.-i..an a.f.p-6 . In 1970 V~. Lou.bat WM -i..nvUe.d
baek to Ge.ne.va M a R.e.~~ -i..n the. 6u.mmeJt
.6eme6t~ .
V~. Lou.bat pMtie-i..pa.;te.d -i..n an
oee.anog~aph-i..e expedition -i..n 1971 6o~ the.

Canad-i..an Oee.anog~aph-i..e I Mt-Uu.te. . The. p~o j e.et
ea.f.R.e.d "deep d~" WM u.ndeJttaken -i..n the.
Sou.th Atf.antie. S-i..nee. eom-i..n9 to Lakehead
Un-i..veM~Ij , V~. Lou.bat hM done. ~e..6e~eh on
we.ak.e.y metamo~phMe.d Mehean ~oek -i..n No~h­
We.6t~n On.:t.a.JUo , a.6 well a6 a the.o~y on the.
ge.ne6-i.6 o6 pe.gm~e. .

�!GEOLOGY LABORATORY TECHNICIANS I
Ann Sumpter
Ann was born and educated in England and
emigrated to Canada in June 1967. She
joined the staff of the Department of
Geology at Lakehead University in July
1968 .
Ann maintains all the requirements of the
first year teaching laboratory and manufactures thin sections of suites of rocks
for all the department ' s teaching purposes,
of students field trip collections and
for the research projects of the Faculty
members .,

Ann Sumpter

(Peppermint Patti)
Pat was born and educated in Thunder Bay
and has been employed in the Department
of Geology for the past 7~ years . She
has a wide variety of skills in the
secretarial, sedimentological , geochemical and petrological fields . Pat
incorporates two interests in one;
that of a professional typist and the
other as a geological technician. Pat
is also well known for her social conventions, eg . Hallowe ' en.

Pat Zurkan

�Ronald Bennett
Chief Laboratory Technician , 1936 to 1967 ,
The Grant Institute of Geology ,
University of Edinburgh .
Research , many kinds of technical approaches
to Ph . D. studies.
Presently, Principal Technician , Lakehead
University .

R.L. Bennett

Sam Spivak
Sam was born in Port Arthur where he
received his basic drafting techniques
in high school and his geological
training while in the employment (for
8 years) of a local mining company and
has been draftsman for the Science
departments for the past '~ years . He
maintains a fairly extensive map library
while drafting time is largely devoted
to preparing maps , overlays and drawings
for use as teaching aids and research
publications.

S.T. Spivak

�Ain Raitsakas
Resident Seismology Affiliate &amp; Mentor
(Alternate Title - The Lure of Seismology)
Ain was born in England some years ago,
emigrated to Kanada several years later
where he has remained even until this
day .
As a graduate of the prestigious Port
Arthur Collegiate Institute , with the
promise of an illustrious career ahead ,
he studied Physics at the University of
Waterloo . He then advanced to Lakehead
University; assimilating knowledge ,
working as a research assistant in Biology , before settling down in Seismology.

A. Raitsakas

Howard Poulsen
Early History: Born, raised and educated
educated in Thunder Bay area .
Education : B. Sc . Physics (1968-1970),
University of Waterloo; B. Sc . Geology (1972), Lakehead University .
Jobs :

Exploration Geophysics (1961-1971),
High School Teaching (1968- 1969) ,
J. M. Franklin ' s right hand man
(1972-1975) .

Interests: Metallogeny, Exploration Geophysics , Evolution of the Archean ,
Keweenawan Stratigraphy, Farming .

K. H. Poulsen

�Jean Helliwell
I was born and raised in Toronto ' the good '
where I comp l eted my High School education
and then a Secretarial course at Ryerson
College . Came to the great Northwest in
1967 and for the past 8 years have held the
position of Geology Departmental Secretary.

Jean Helliwell

T HA NK

y0u

TO

DR, M. BARTLEY

- HoNORARY PROFESSOR, LA KEHEAD UNIV ERSITY

MR S, J, HELLIWELL - SECRETARY, GEOLOGY DEPARTMENT
MR.

i
I

s. SPIVAK

MISS P. ZURKAN

- DRAFTSMAN, GEOLOGY DE PARTMENT
- LAB TECHNI CIAN, GEOLOGY DEPARTMENT

���environ mental
contro-1
40years ago
One of the finest recreational parks in Northern Ontario
is located between the old Hollinger mine and the adjoining
town of Timmins, a Northern Ontario mining community
of 30,000 people. When the Hollinger mine and Timmins
were both young the park was a tailings dump in a shallow
lake, unsightly and dusty.
More than 40 years ago-long before environmental control
became a subject of public concern-the dump was
converted into a public park, maintained by Hollinger.
It provides facilities for baseball , soccer, track and
field events, picnics, field days, concerts and other
recreational activities.
When the Hollinger mine closed, the park was ceded to
the town of Timmins, but it remains a symbol of Hollinger's
long-held belief that a successful mining operation can
and should enrich the lives of all Canadians. It also
provides enduring evidence that the need for
environmental control was accepted by Hollinger long
before the subject became publicly popular.

HOLLINGER MINES LIMITED

�Canadian Exploration OHices
Su1te 1302 - 7 King Street East

TORONTO, ONTARIO MSC 1A2
(416 364-6188

EXPLORATION , INC.

601 - 53 5 Thurlow Street

VANCOUVER, B.C. V6E 3L2

EXPLORATION
EVALUATION
DEVELOPMENT
FINANCING

(604) 683-0474

P 0 Box 1150
TIMMINS, ONTARIO P4N 7H9

(705) 264-5247

1666 Dublin Avenue
A Subsidiary of:

WINNIPEG, MANITOBA R3H OH1

(204) 786.4881

PO Box 130

AMERICAN METAL CLIMAX, INC.

STEWIACKE, N.S. BON 2JO

(902) 378-2603

SIIIP HOCK IRON MINIS liMIIID

~~~k.de
LAKEHEAD UNIVERSITY GEOLOGY CLUB
SUIP HOCK IRON MINIS liMIJID
Atikokan , Ontario

��\Vecanhelp
make it happen.
If you would like advice or information on
any of our helpful services, why not drop
in soon. We'll be pleased to help you in
any way we can.

serving Ontario

�EDITOR'S MESSAGE
This year book has been approximately
three years in the making.
During that time people
have come and gone.
Due to this turnover there
have been many changes made, both in material and
year book staff.
When I and a few other concerned
students took over,what faced us was an unorganized
attempt of putting together a Year Book . We have
attempted to put what pieces we had into some
semblance of order. We have made no attempt to
update the material to any great extent in order to
finally get this year book done.
Due to thi s many
important details have been left out.
material

Thus I wi 11 give a brief resume of this
that was left out of the Year Book .

To begin with I will start with the
faculty.
In the winter of 1973/74 Dr. H. Loubat
resigned his position at Lakehead and is now
teaching in Quebec.
Dr. Garth Platt was hired to
fill this vacancy in the fall of 1974.
This spring Dr. Jim Frankl in was offered
a position with the Geological Survey of Canada which
he has accepted.
My only comment here is that L.U.
Geology has lost one of its finest members .
Listed below are the names of all the
Geology students from 1974/75.
I am sorry that no
pictures of many of these students are available
a nd my a p o 1o g i e s f o r t h i s fa i 1 i n g o n t h e p a r t o f t h e
past year book staffs.
FIRST YEAR
Herb Christmas
Brian Cole
Douglas Cole
James Crinklaw
Ernest Grach
Randy Ha 11
E 1 i zabeth Johnston
Alan Koskela
Fred Peters
Jeffrey Record
Jean Samson
Bernard Schnieders
Frank See! iger
Mark Wittrup
Gordon Yule

�SECOND YEAR
Alan Aubut
Frank Balint
Kenneth Hartviksen
Stephen Hitchman
Eric Mosley
Donald Nicol
Keith Peden
Randy St. Jacques
Ronald Tapsay
Donald Turubchuk
Gerald Varteniuk
THIRD YEAR
John Biczok
Heather Boyle
George Chabot
Albert Chiew
William French
Holly Johnston
William Mclellan
Gerald Perry
Frank Smit
The following is the names of the students
in the FOURTH YEAR - HONORS DEGREE for 1974/75 and
also their thesis titles.
DENIS BATTRUM

Sedimentology of the Kama Hill
for mati o n o f th e Sibley Group .

JACK CLUE

The formation of stream ripples.

GARY GRABOWSKI

Geology of the Atikokan iron mine.

WILLIAM HODGINS

Selenium absorption of Mn02.

DENNIS KWIATKOWSKI - Geology and geochemistry of
anthraxol i te.
DOUG LEHTO

Structural and petrological
evo luti o n of th e Do g-Hawk eye Lake s
area.

�JOHN MASON

Quaternary sedimenology and
stratigraphy of Thunder Bay.

WILLIAM MCRAE

Determination of cesium by
neutron-activation analysis.

MARIO SILVA

Internal structure and petrology of the Trout Lake Intrusion.

GORDON STEINERT

Structure and petrology of the
Barnum Lake quartz-monzonite.

JAMES SYVITSKI

Element concentration of the
waters and sediments of Thunder Bay.

The next 1 ists are the names plus thesis
titles for those students that have graduated in
1973 and 1974, in that order.

1973

HONORS DEGREE

BRENT PASKE

Geology and geochemistry of the
Onaman Lake Property, Northwestern
Ontario.

GEORGE EINARSON

Variations in the style of Metamorphism in Archean Supracrustal
Units of the Superior Province.

ROBERT KYRYLUK

Description of structures and their
significance in a migmatite complex.

LESLIE TIHOR

Archean evolution of Western
Dorion township.

ALLAN SPEED

The investigation into the use of
gamma-ray spectrometry as a possible
geologic mapping tool.

JOE KASARDA

Wall-rock alteration and trace element
geochemistry of the footwall rocks of
the Mattabi Deposit, Sturgeon Lake
area .

NEIL CAMPLING

Some geological and environmental
aspects of remnant pre-Gunflint and
pre-Sibley weathered profiles.

�What comes

out ofa Mine?
What comes out of a mine? Minerals, of course.
But much more than minerals ... such as:
Jobs- at the mine sites- thousands of them.
Jobs- in industries supplying goods and ~ ... ·vices
to the mines- hundreds of thousands of them.
Exports- about 1/3 of the exports required by Canada to maintain its role as a senior trading
nation.
New communities- there are hundreds of mining
communities across Canada.
New opportunities in new communities -for almost
every kind of trade, skill , profession, talent or
business.
New wealth- total value of Canadian mineral production in 1973 exceeded $8 billion -wealth
translated into the Canadian economy for
wages, salaries, supplies, services, taxes and
dividends.
The Canadian mining industry is a valuable,
useful industry in Canada - valuable and useful enough to be studied, understood and
encouraged.

HOLLINGER MINES LIMITED
Labrador Mining
and Exploration
Company Limited

Hollinger North Shore
Exploration
Company, Limited

�heath &amp;sherwood drilling
A Division of

•
•
•
•

~C "

Upper Canada Resources Limited

Diamond Drilling
Dual Tube - Overburden sampling
Chip Sampling
Deep Hole Rigs
Unitized, Skid and Mobile Rigs

KIRKLAND LAKE

SUDBURY

THUNDER BAY

TORONTO

WIN NIPEG

705-567-9311

705-682-2833

807-577-9043

416 -364-7301

204-889-7369

Head Office -

908 - 40

University Avenue

Toronto, Ontario M5J ITI
Member Canadian Diamond Dnlling Assoc1at1on

THE

PAS

204-623-2722

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1977 - 78

Bruce Jogo

Heother Brouun

Sditor

Co-£ditor

4

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Edition

�CONGRATULATIONS AND
to the

M. W. BARTLEY

BEST

WISHES

Graduates

8

ASSOCIATES

LTD.

Geologists
202

Toronto - Dominion

Thunder

Bonk

Bldg.

Bay, Ontario

noranda
Noranda Exploration Company, Limited
no personal

liability

Branch Office

253

Lincoln St.

Thunder Bay

J^ottk IVeSt J4^%aulic3

J^td.

TELEPHONE 622-5809

ROLAND STREET
BOX 955, STATION P
THUNDER BAY. ONTARIO
1095

P.O.

P7B 5G5

Budget
rentacar

^HHHI

R.

J.

TVRNER
BUDGET RENT-A-CAR OF THUNDER BA Y
219 West Gore St.,
Thunder Bay, Ontario

Phone

-

Office 577-7571

�Dedication

This fourth volume of the Geology Yearbook is dedicated to the spirit of

Sir William Logan

a pioneer in the investigation of Canadian geology.
In 1843 an Act of the
Provincial Government of Canada (the union of Lower and Upper Canada, formalized in 1840) established the Geological Survey of Canada, with its headquarters
in Montreal, the Provincial Capital.
Under the direction of Logan an enormous
amount of work was completed by him and his colleagues so that in 1863 he was
able to see the publication of the monumental ’Geology of Canada' and the first
Geological Map of Canada. His own researches are a measure of the stature of
the man - explorations in the Lake Superior region north of Lake Huron and aalong the
long the Ottawa Valley with the Mattawa Valley to Lake Nipissing;
St. Lawrence Valley in Quebec, in the Eastern Townships and in the Gaspe Penninsula

In the history of our country the Geological Survey has a prominent place
in the flourishing present and is founded on a glorious past, because of the
spirit of men like Logan. The promise of the future is in other hands, such as
those that produced this Yearbook, but that future is assured as long as the
memory of our great fellow countrymen lives on.

�Compliments from the

office of the President

Lakehead University

Dr.

A.D.

Booth

�FINNISH

and

CANADIAN

DISHES

Good Food

Low

Prices

HOITO RESTAURANT
Open

Monday

- Friday

Saturday &amp; Sunday
314

Bay

Street

6:00 am
8:00 am

-

8:00

-

8:00

pm
pm
345-6323

Expresfway Lounge
LANDMARK
(807

-

767 - 1681

)

County Fair Plaza

INN

�Compliments of the

Faculty of Science

Lakehead University

�Message from the President

I

success both

wish the 1911 / 1 ^ crop of Geology students
in their studies

and

in their future

Lakehead University every

at

On successful graduation,

careers.

they are one of those relatively small groups of university graduates who will find no
difficulty in obtaining suitable

The future

of the

employment.

world, both as regards energy and other mineral resources,

depends on renewed and extensive geological exploration and development.

Likewise,

the future of the smaller towns of Northwestern Ontario, as well as those elsewhere,

depends on the discovery of new resources

It is

also

at large, that at last

my pleasure
it

by the local inhabitants.

Geology students, as well as the public

appears that we have overcome the hurdles

menting our Master of Science
luck, this should

to tell the

to be exploited

in

come on-stream

Geology course

at

in the

Lakehead University.

way

of imple-

With any

for the session 1978/79, and best wishes and thanks

go to the Faculty and Staff who have helped to make this regionally-relevant idea a
practical possibility, as well as to the National Research Council whose generous

funding for this development overcame the financial obstacles.

ANDREW

D.

BOOTH, Pr^ident.

�Message from the

Dean of Science

I

would like to congratulate the Editor and Staff

for their initiative in recommencing the Geology Year Book

series

The primary purpose of students whom enroll in a

programme of study at a university should be to obtain an
However, a university experience should consist

education.

of more than lectures, laboratories and examinations.

It

should be a time when young people undergo considerable
social and cultural development.

The comradship involved

in bringing the Year Book to a successful completion is part

of this extracurricular experience.

I

wish the members of the Geology Club a rewarding

and successful sojourn at Lakehead University.

Best wishes!

JOHN S. MOTHERSILL,
Dean of Science.

�Message from the Chairman
"I take things such as I find them at present^ and from there I
reason with regard to that which must have been
.

.

(James Hutton 1726-1797

In the past year a number of developments have taken place which will have
an effect on everyone in the Geology Department at Lakehead University. Revisions in the undergraduate programmes and courses were completed. With these
changes we believe that our students will be exposed to a more competitive
programme which will prepare them for a variety of alternatives upon graduation.

In the coming year the Department will embark on its graduate programme
which was recently approved by the Council of Ontario Universities. It has
taken a great deal of hard work and an even greater amount of patience over many
years which now make it possible to provide students the opportunity of a graduate programme in Geology at Lakehead University. Graduate research topics
will focus on the Precambrian of the western Superior Province and adjacent regions, and will be centered in the major disciplines of Geology.
The presence
of graduate students will be of benefit to all of us, for they will form an
Integral part of the geological family at Lakehead University.
The geological community at large will also experience some significant
changes in the next few years. A major portion of the Geological Survey of
Canada will be relocated in Thunder Bay by 1980. Among the geologists to be
transferred here are members of the Precambrian Division, the Petrology, Geochronology, and Paleomagnetlsm Sections. The Impact of this explosive increase in the geological community is difficult to imagine in all its ramifications. Whatever the outcome, it remains certain that for us all it will provide a previously nearly non-existant setting in which we can readily exchange
geological knowledge and ideas. Such an environment will surely enhance the
present high level of research activity.
In the next few years we will experience the full impact of these changes.
In the meantime there remains much for us all to do to ensure that we will benefit the utmost from these developments. May I extend my heartiest congratulations
and admiration to all geology students on the successful production of the Geology
Yearbook. You have shown yourselves capable of imagination, initiative, boundless energy and perslstance in this worthy undertaking. Your labours will serve
future Yearbook organizers well. On behalf of the Geology Department I extend
our best wishes to you in your future endeavours.

M.M. Kehlenbeck,

Chairman

�G

��Dr. John S. Mothersill. B.Sc.. B.Sc.. Ph.D.

Background;
Exploration Geologist for Standard Oil (N.J.)
Senior Geologist for Mobil International Oil Co.
Exploring for petroleum in Turkey, Nigeria, France
and Colombia, 1956-64
Associate Professor, Lakehead University, since 1966
Dean of Science at Lakehead since 1975.

During June, four Alpine piston cores were taken of the sedimentary
sequence in the main post-glacial basin of Thunder Bay from a Deep Diving
Systems drilling barge. The locations of the cores were picked so that increasingly thicker post-glacial sections would be encountered from the basin
margin toward the basin centre. All four cores consisted of the underlying
glacial varved section.
Seven hundred and eighty— four oriented, two— cm^ samples were taken
from along the length of three of the cores (at 3 cm intervals throughout
the post-glacial section and at 10 cm intervals throughout the varved section).
The declination, inclination, intensity and susceptibility of magnetization
and Q ratio (intensity/ susceptibility) of each sample was determined using
paleomagnetic equipment at the University of Edinburgh. These data were
plotted by computer programme and the declination direction variations were
correlated for the two thicker post-glacial section cores. For the postglacial section, five major swiggs occur in declination; the inclination
variation is in the order of 35 ; and the susceptibility shows two slight
but significant shifts. The uppermost susceptibility shift appears to correspond to the time of the Nipissing phase based on radiocarbon age determinations. Substantial decreases in the intensity and susceptibility of
magnetization were noted for the sediments at the base of the post-glacial
section. Paleomagnetic directions also were determined after the samples were
"cleaned" in a peak field of 200 oersteds to get rid of any extraneous NRM
directions. The declination and inclination determinations of the cleaned
samples correspond almost identically with the results obtained from the uncleaned samples. Radiocarbon analyses are being carried out on fifteen
samples from two of the cores to determine the age of the declination and
inclination swings and susceptibility shifts. This age-dated paleomagnetic
column will be used for time-parallel correlations throughout the northern and
western Lake Superior area. Post-glacial sediments in this basin should
provide a continuous or near continuous sedimentary record to assess sedimentation rates and climate changes. Presently, sedimentation rates are being
assessed by; a)
determinations, b) the variability of the organic C/N
content of the samples after treatment with sulphurous acid using a PerkinElmer CRN Analyzer and c) grain-size variability using the Micromeritics
Sedigraph 5000 method. These data are presently being compiled.

During the summer, a report in methodology for determining asbestos
fibre counts Irl water was finalized in conjunction with co-workers from several other laboratories in the province. The method will be recommended to the
Ministry of the Environment (Ontario) as the standard method for determining
asbestos fibre counts in water.

�Dr. Edward Mercy, B.Sc., Ph.D^, D.I.C,
Academic Background;
Lecturer in Geology, Imperial College of
Science and Technology, London, England,
Lecturer in Geology, later Senior Lecturer
in Geology, University of Edinburgh, Scotland.
Professor of Geology and Chairman of the
Department, Lakehead University, 1967-1976
Professor of Geology at Lakehead since 1976.

I

was granted sabbatical leave by the University for the academic year

1976-77, a welcome break after nine years of administration. The purpose of
a sabbatical leave is to relieve the faculty member of his teaching and admin-

istration functions and so enable him to renew his primary scholarly interests.

Many use the time to develop and strengthen their research work, others write
the book they have been thinking about for years. My need was overwhelmingly
to catch up on my reading.

It is a truism that scientific knowledge is expanding at an explosive

rate and that scientists are becoming more and more specialized. In my own
field of geochemistry the explosion of knowledge and understanding has been

triggered by the great advances in analytical capability brought about by
the new science of electronics, without benefit of which my generation did

their research work. I am now aware that I can do no more than keep abreast
of the new knowledge by reading and dedicated study. It is a major task to

separate the dross, of which the system encourages more than is at all reasonable, from the reality of truly new work and insight. My earnest hope is that

by continuing study and appraisal my teaching functions, surely the most

important aspect of a university professor, may be done at the highest possible level of attainment.

�Dr. Manfred M. Kehlenbeck, B.A., M.S., Ph.D.
Academic Background;
Visiting Professor, University of New Brunswick
1969-70
Teaching Fellow, Queen's University 1970-71
Assistant Professor, Lakehead University 1971Chairman of the Department of Geology, Lakehead
University since 1976.

The western part of the Superior province is composed of a series
of subprovinces which have become better known as belts. Among these
structural subprovinces are the Quetico, Shebandowan, and Wabigoon
belts.
In the area north of Thunder Bay these belts are well
exposed, and the rocks within them have been the substance of my
research interest for the past six summer seasons.

Although my interests range widely, I have become Increasingly
more concerned with the spatial and temporal relationships of the rock
types of adjacent belts.
The Quetico Belt in particular, has held my
fascination because it is bounded on the south by the Shebandowan belt
and on the north by the Wabigoon belt and therefore offers a perfect
target to study the relationships between three adjacent belts.
Structurally the Quetico belt is characterized by linear and, to
planar elements which produce a dominant east-west
grain. These same structural elements in the adjacent belts appear more
varied in attitude except near boundaries with the Quetico belt where a
zone of transition forms the changeover to the dominant east-west trend
of the Quetico belt.
a lesser extent,

Studies of the lithologies exposed in different belts have shown
The metamorphic
that essentially similar rock types occur in all the belts.
history differs between belts so that the rocks tend to appear different
at first glance. Relative abundances of rock types also vary from belt to
belt as well as within a single belt.
It appears certain that the structural characteristics are among the
important criteria by which we can divide the western Superior province
into subprovinces or belts.
What now appears essential is to establish
a tectonic framework which will explain the reasons for the observable
structural differences in portions of the Archean crust.

i;

�Dr. M.W« Bartley, M.Sc., Ph.D.

Backgroundj
Lecturer University of Toronto 1938-40
Iron Ore Exploration since 1938
Steep Rock Iron Mines development 1940-48
Principal, Lakehead Technical Institute
1948-52
Honary Professor Lakehead University
since 1971
President C.I.M. 1976

I am one of the fortunate people who has had a very rewarding experience being involved with mineral exploration, mine development, mine
operations and academic endeavours for almost forty-five years.

My greatest reward has been the accumulation of many close friends
and professional peers, young and old in many parts of the world. Nothing
can take the place of friends in one's chosen field of endeavour because
they are always a source of enjoyment and a limitless fund of information.
I maintain that whatever success I may have had is not the result of what
I know but rather who I know and can turn to for advice.
After graduation from the University of Manitoba in 1934 and during
subsequent post-graduate work I was employed by the Ontario Department
of Mines during the field seasons and lectured at the University of
Toronto during the academic year. During my final year of post-graduate
work at Toronto I enlisted in the R.C.A.F. but was seconded to Steep
Rock Iron Mines Limited to develop an iron mine in support of the war
effort.
I have remained in the field of iron ore exploration and
development since that time. Interspersed was a brief period, 1948 to 1952
as Principal, Lakehead Technical Institute.
My, involvement in the consulting field has been very pleasant and
educational. My work has taken me to every Province except Prince
Edward Island, to many of the United States, to the high Arctic and to
Each has
several countries in South America, Asia, Europe and Africa.
been a new experience and I can recommend the life and the role to all
graduates in geology.

Since I have lost the desire to attempt fifteen to twenty mile
daily mapping traverses my present endeavours are directed towards
economic appraisals and evaluations of mineral deposits and mine development. These are exacting assignments, often fraut with frustration
I find
because of the vast bureaucratic maze which must be negotiated.
that my few hours per week devoted to Instruction at Lakehead University
I enjoy sharing my experiences with students who
is a welcome respite.
are so eager to learn and are so appreciative of assistance.
I heartily recommend that all prospective geologists and those in
allied sciences become members of professional associations. It is through
these affiliations that you will gain professional stature and lasting
personal satisfaction.
I wish you success, satisfaction and many years of productive life
after graduation.

�Dr. Roger H. Mitchell, B.Sc., M.Sc., Ph.D.

Academic Background;
Lecturer in Isotope Geochemistry,
University of Oslo, Norway, 1971-72.
Assistant Professor of Geology,
Lakehead University, 1972-76.
Associate Professor of Geology,
Lakehead University, since 1976.

Field work this year commenced with a visit to the "Moonshine Hills" of
Kentucky in search of the type locality of mica peridotite. The search was
not a resounding success as the peridotite dikes are intruded into faults
occupied by flourite veins which weather to a persistant glutinous red mud,
thus hiding the igneous rocks. Six months later I still have some of the mud
on my boots. Samples were found with the aid of gophers, despite such hazards
as flourite mud, bloodsucking ticks, snakes, fields of poison ivy and a local
populace remeniscent of characters from "Deliverance". Never do field work
in Kentucky unless you really have to
I

Springtime found myself as 100% of the crew of the notorious Captain
Platt and involved in a study of the igneous rocks found in the Lake Superior
Islands and of the nepheline syenites found on the Marathon Riviera - field
work not to be missed if you ever get the chance - one of the most beautiful
parts of Lake Superior.
July found Dr. Platt and myself encamped upon some awfully stoney
ground in the permafrost desert called Bathurst Island. Our work there
sponsored by the Federal Polar Continental Shelf Project, was to make a detailed study of the Freeman's Cove volcanic rocks, these are the second only
known occurrence of nephelinite in North America. During the work Dr. Platt
did an excellent job as gunbearer, wreaking havoc amongst the oil drums with
the 30-06, but failed abyssmally in attracting any polar bears. In fact, the
fiercest beast we came across was a long-tailed jaegar.
The fall saw me once more in the desert, but this time in the very hot
Arizona desert. As a part of the Second International Kimberlite Conference
field trips were organized in the U.S„ southwest. Here I collected kimberlites,
minettes and pieces of mantle to compliment my studies of Canadian and South
African upper mantle material. Much of the field work involved such activities
as pushing rubber rafts down the San Juan River Canyon, climbing mountains
under the blistering hot sun or coughing ones way around sagebrush and cactus
in sandstorms. All very enjoyable and some 70 petrologists were kept on the
liquidus by consuming some 5000 cans of beer over ten days. In all this was
the most Interesting field work of the year as I saw recent volcanism, the
Grand Canyon, Monument Valley, the Rio Grande Rift, and a wide variety of
igneous rocks.

�Dr. R. Garth Platt, B.Sc.. Ph.D.
Academic Background;
Visiting Professor, University of Copenhagen,
Denmark, 1969-70
NRC Postdoctoral Fellow, University of
Western Ontario, 1970-71.
N.E.R.C. Research Fellow and Staff member.
University of Edinburgh, Scotland, 1971-74.
Assistant Professor, Lakehead University,
since 1974

The "summer" season began and ended with organized field trips to the

Coldwell Alkaline Complex in N.W. Ontario. The early summer field trip was
organized for the 23rd Annual Meeting of the Institute on Lake Superior
Geology. A guide book was prepared for the occasion. The late summer trip
saw a group of hardy students (some students claimed it snowed - fertile

imaginations), studying the complexities of North America's largest alkaline

complex and the rigours of life on

the North Shore of Lake Superior.

In between these events, serious research was continued on the pet-

rology of the Coldwell Alkaline Complex with particular emphasis on the nepheline syenites and the dike rocks associated with the intrusion. In addition,

preliminary investigations of the Keweenawan Osier Volcanics of Northwestern
Ontario were undertaken. The department's research boat was often seen braving
the waters of Lake Superior with Dr. Platt in command and Dr. Mitchell navig-

ating.

Dr. Mitchell's navigation was so bad that the beginning of July saw us

both on Bathurst Island in N.W.T.. This trip, under the auspices of the Polar

Continental Shelf Project, was made to initiate studies into the geology
and petrology of the Freeman's Cove Alkaline Volcanic Suite. This suite, containing as it does, nephellnites, basanites and phonolites is unique to the

Canadian Arctic and its study will provide us with valuable information about
the geological history of the area.

�Dr. Stephen A. Klssin, B.Sc., M.S., Ph.D.
Academic Background;
Post Doctoral Fellow, McMaster University 1973
N.R.C. Post Doctoral Fellow, CANMET, Department
of Energy, Mines and Resources, Ottawa 1974-75
Assistant Professor, Department of Geology,
Lakehead University since 1975.

My activities last summer began with the GACMACGEGCGU (basically.
Geological Association of Canada / Mlneraloglcal Association of Canada)
meeting in Vancouver in late April. As well as presenting* a paper on
the new mineral cernyite, Cu CdSnS
I attended a field trip to the
,
southeastern B.C. lead-zinc deposits. My particular aim was to collect
specimens from the Sullivan Mine, with the view of examining the tin
mineralogy and pyrrhotite-sphalerite geobarometry.
On my return to Thunder Bay, I was involved with the 23rd Annual
Meeting of the Institute of Lake Superior Geology, hosted by the
Department, in the capacity of Technical Sessions Co-Chairman. I also
attended the Mattabi field trip as a supernumary. For the remainder
of May, I worked on the preparation of journal papers and some geological
field problems in the Rabbit Mountain Mine area. My efforts were
interrupted by the birth of my daughter, my second child, on May 31st.
After two weeks at home, I returned to the University to work on
another journal paper on stannite and other tin-bearing sulphide
minerals. Continued study on tin-bearing sulphide minerals led me to
One
the appreciation that two previously undiscovered species exist.
is the cubic form of stannite, normally tetragonal Cu FeSnS^, while the
2
other is the iron analogue of kesterite, Cu 2 ZnSnS , which is also
tetragonal, but has a space group which differs from that of stannite.
In the latter part of August, I spent some time in the field mainly
in the reconnaissance study of silver mines in the Rabbit Mountain area.
As well, I made a trip to Ottawa to use the facilities at CANMET in
order to investigate the two new minerals mentioned earlier and continue
some aspects of research on the synthetic system Cu 2 FeSnS^-Cu 2 ZnSnS 4
After all this, I found that the summer was suddenly gone.
.

F
1

�Roy J. Shegelskl, H.B.Sc., M.S., Ph,D.
(pending)

Academic Background;
University of Toronto 1973-77
Ph.D. pending
Lecturer at Lakehead University
since 1976

This summer was spent investigating mafic volcanic terrains in the

Northwest Territories. The particular areas of study were the Nowyak Lake
area and the Griffin Lake area which are within 60 km of each other and

located in NTS sector 65G. The areas are located within the Churchill Pro-

vince and are Archean in age. The predominant lithologies of the areas
include pillowed and massive basalts with subordinate amounts of ultramafic
flows

(

some showing splnifex textures), banded and laminated oxide facies

iron formations, chertz sulphide facies iron formations and minor felsic

pyroclastic and volcanoclastic tuffs and sediments. These areas were being
investigated for massive sulphide potential. Results of the follow up to

geophysical airborne and ground surveys in one of the areas led to the delineation of several favourable zones of nickel sulphide mineralization, in
fact results are so encouraging that I cannot talk of them I The summer was

relatively wet; the black flies were bad but the crews were great and included
two able assistants from L.U.; R. Hall and B. Schneiders

1

�1

Howard Poulsen. B.Sc. (Physics), B.Sc. (Geology')
Background;
Exploration Geophysics 1961-71
High School Teacher 1968-69
Research Assistant (for J.M, Franklin) 1972-75
Laboratory Demonstrator at Lakehead
University since 1975

In addition to the ongoing analytical work of the Geochemistry Lab,
the past summer provided for me three geological highlights; the annual
meeting of the Institute on Lake Superior Geology in May; the visit of
three foreign students at our Department; and a major retrieval of soft
sediment cores from Lake Superior.

My contribution to the LSI meeting centered around a 2-day postconference field trip to the Mattabl and NBU massive sulphide deposits.
The trip, which entertained 46 geologists from all parts of North America,
stressed the geological setting and genesis of the deposits based on
the research of James Franklin of the Geological Survey of Canada.
Jim
and I spent a good deal of time organizing the trip in conjunction with
the mine geologists as well as preparing a trip guidebook which summarized
much of our research work at Sturgeon Lake carried out in the interval
1972-75.
The summer saw the arrival of three graduate students from GeologischPaleontologisches Institut, University of Hamburg, West Germany. Frank,
Rudi and Claus had come to Thunder Bay to study iron formations as part
of their graduate thesis requirements at Hamburg and informally allied
themselves with our Department for the summer. Their stay here provided
many interesting insights into geological education in Germany in comparison with the type of programme offered by our own University. Of
particular interest was their reason for coming to Canada for field work;
they had the sinking feeling that possible hundreds of geologists
had already worked on most of the exposures in Germany. Our own fourth
year students can take heart from this, considering the novel field aspect
of most of their bachelor's theses.

One particularly fine sunny day found me aboard a barge in the middle
of Thunder Bay harbour as part of a crew Involved in the retrieval of
four 50 foot piston cores of lake bottom sediment.
The project was
headed by Dr. Mothersill who is using the materials collected to study
various aspects of the evolution of Lake Superior during the past 12,000
years. Although this project was of short duration ( one day ), it was

most enjoyable and

I

didn't even get sea sick.

1

v'

�Rona Id Bennett

Ron was the Chief Laboratory Technician
at the Grant Institute of Geology, University
of Edinburgh from 1936 to 1967. His research
includes many kinds of technical approaches
to Ph.D. studies. He has been the Principal
Technician at Lakehead University since 1967.

Ann Sumpter

I

I

Ann was born and educated in England and
emigrated to Canada in June 1967. She
joined the staff of the Department of
Geology at Lakehead University in July 1968.
Ann maintains all the requirements of the
first year teaching laboratory and manufactures thin sections of suites of rocks
for all the Department's teaching purposes,
of students field trip collections and
for the research projects of the Faculty members.

Sam Splvak

Sam was born in Port Arthur where he
received his basic drafting techniques
in high school and his geological
training while in the employment (for
8 years) of a local mining company. He
has been draftsman for the Science
Department for the past 7^5 years. He
maintains a fairly extensive map library
(4500 geological maps), while his drafting
time is largely devoted to preparing maps,
overlays and drawings for use as teaching
aids and research publications.

�Pat Murphy

Pat was born and educated in Thunder
Bay and has been employed in the Geology
Department for the past 9% years. She has a
a wide variety of skills in the secretarial,

sedimentological, geochemical and petrological
fields. Before becoming secretary to the
Dean of Science, Pat was a professional
typist as well as a geological technician.

Ain Raltsakas
Resident Seismology Technician, Ain was
born in England a lifetime ago. His emigration to Canada at an early age was briefly
marred by his kidnapping and subsequent
release by extra-terrestrials from Ganymede (who, incidentally, refused ransom).
He was educated in Physics and the ways
of the world at P.A.C.I., the University
of Waterloo and Lakehead University where
he won (?) a B.Sc. in Eclectic Pretensions.
Prior to joining the Geology Department
in 1973, he was engaged as a researcher
of mycorhizal relationships. He presently maintains the various functions of
the Lakehead Seismographic Station
and all that that entails.

Wendy Bons
Wendy is originally from the
Toronto area where she received her
high school and college education.
She has spent the past 3h years in
Thunder Bay, the last year being
spent in the Geology Department
as the Departmental Secretary.
Secretarial duties in the Geology
Department include such things as
typing, filing, handling of incoming
and outgoing calls, departmental
budget documentation and documentation of faculty N.R.C. grants.

�THE WILEY STREET GANG
a

the

Revue boasts:

•certified

• buy and sell

G. Turner

,

,

G. Yule

• T-shirt

Prospector

&amp;

• contract staking

B. Cole

itecci

(

OK

sales

(division of

• charitable

linecutting

•

used snowshoes

phone

:

345

-

6220

Gereburn)

beer disposal outlet

A

class (y) mechanic

)

Mattagami Lake Mines Limited
Exploration

Division

NORTHWESTERN FIELD OFFICE
PO.

THUNDER

BOX

2326

BAY,

ONTARIO

TELEPHONE

344-8312

P7B 5E3

Wishing every success to all the members
of the Lakehead University Geology Club.
-

AAAAIC

Canadian Exploration Offices:

Suite 1302
7

IS

King Street East

TORONTO, ONT. M5C 1A2

EXPLORATION
EVALUATION

DEVELOPMENT

(416) 364-6188

601

-

535 Thurlow Street

VANCOUVER,

B.C.

V6E 3L2

(604) 683-0474

FINANCING
P,0.

AIWIAH
MINERALS EXPLORATION
(A Division of

AMAX POTASH

LIMITED)

Box 1150

TIMMINS, ONTARIO P4N 7H9
(705) 264-5247

P O

Box 510
SACKVILLE, N.B. EOA SCO
(506) 536-2278

���WE THE WILLING, LED BY THE UNKNOWING,

ARE DOING THE IMPOSSIBLE, FOR THE UNGRATEFUL.
WE HAVE DONE SO MUCH FOR SO LONG, WITH SO LITTLE,

WE ARE NOW QUALIFIED TO DO ANYTHING WITH
nothing:

�Future Geologists

I.U. s

The product of four years in Geology at L.U. From left to right; Bernie Schnieders,
Keith Peden, Gord Turner, Randy Hall, Brian Cole, Roman Tykajlo, Maureen Morrison,
Tim Manilla, Gord Yule, Mark Wittrup.

It's north to Alaska guys,
.or is that the Crest?
.

.

.

�Brian Cole
Nickname: Wimp First Class
Pet Peeve: Eggshells in the sink.
Favourite Exp: 'Turner you gink'
Work Experience:Recon. (Junior) mapping.
Geochemical Sampling
Falconbridge Nickel, Summer 76
Contract Geochemical Sampling,
Winter 1976
Recon. (Senior) mapping. Airborne
geochem. and geophysics.
Summer 1977

Brian is a member of the Wiley Street Revue.
ite activity is fixing a certain 1970 Far-gone.

His favour-

Brian usually

plays squash and outruns Ron with the coffee pot for exercise.
In between playing with his rocks, Brian attends all his

classes.
Lab.

He spends all of his free time in the Mineral Deposits

Upon successful completion of 4th year Brian hopes to become a

famed exploration geologist.

Thesis Topic: Geology and Mineralogy of The Beaver Junior Mine

The Beaver Junior Mine is one of the many workings in
the northeast trending mainland belts of silver mines in the

Thunder Bay area.

It is located near the village of Stanley

in the Thunder Bay District.

The study of this mine involved

a descriptive survey of the structure and geology and sampl-

ing for petrographic studies.

Mineralogical investigation was

based primarily on polished and thin section studies.

Geology

was determined from detailed mapping of the vein and various
structures in close proximity to the mine adit.

The final objective of this thesis was to draw conclusions
concerning the paragenesis of this type of deposit.

V

�Maureen (FitzGerald) Morrison
Work Experience: Junior Mapper and Geochemical
Sampler,
Texas Gulf, summer 1977

A pretty small group
In geology here
Frosh know everyone
Right to fourth year

To
To
To
My

Lakehead I came
take Chemistry
go toward
Western degree

Not so at Western
I say with a sigh
But it's still a great place
And I rate it quite high

But soon I was told
L.U. is the best
The Profs are all keen
The students have zest

Sure and why not
They seem to be
A pleasant enough lot

In N.S. and Gaspe
And good old N.B.
In '77 I worked
For Texasgulf-Tg

At Western they're snobs
Or so I was told
Not totally wrong
But pretty damn bold

Junior mapper was I
And an expert soil sampler
Travelling around
In a bright orange camper

So I said to myself

Great fun it was
And I learned some tidbits
To use as I become
An L.U. Geologist

�Randy Hall
Work Experience: Junior Assist. Noranda Yellowknife 1976
Senior Mapper, Noranda Yellowknife 1977
Thesis Topic :Archean Komatiitic Flows of the Henik Lake
Volcanic Terrain

One of the cities famed mini drivers, Randy prides the 4th
year class with his usual presence.

Noted for his helpful person-

ality, Randy enjoys a cold beer while watching slide shows.
of the Pink Paradise tenants,

Another

there is hope someday for a decent

residence

Randy has spent two previous summers with Noranda Yellowknife
office both as a junior and senior Geological Assistant in base

metals exploration.

The north seems to have a strange affect on

people and chances are that Randy may be returning with Noranda
next summer as a Party Leader.

Randy's thesis is basically a study of a series of ultramafic
flows located in the Griffin Lake area of the Keewatin District,

Northwest Territories,

A section of these flows were carefully mapped and sampled,
and the geochemical, textural and mineralogical variations across

individual flows, and changes between successive flows are being
examined
The ultramafic units are also examined in light of the sulphide

mineralization in the region, noting compositional changes and the
mineralogy of the host rock and ore minerals within the map area.
As a result of this work, a composite picture of these

particular spineflx textured flows shall emerge, and some attempts
will be made to compare these flows to other slmiliar units elsewhere
in Archean terrain.

�Tim Manula
Nickname: B. Brother Nurd
Work Experience: Junior assist. Falconbridge 1976
Senior mapper, Gulf (uranium) 1977
Thesis Topic Geology and Mineralogy of the West
Beaver Silver Mine, Thunder Bay
:

Tim is the youngest member of the fourth year entourage.

He is

closely associated with Wimp and Gink and has become affectionately
known as B. Brother Nurd.

His blond hair, blue eyes and big feet

mark him as our representative Lapplander.

His hobbies are also in-

They include cross-country and

dicative of his ethnic background.

downhill skiing, snowmobiling, playing hockey, jumping into Lake
Superior after a sauna in the dead of winter, drinking and herding
reindeer.

At school he engages in activities such as striking days

off on his calendar, complaining about the mechanical fitness of his

VW bus and drinking coffee along with the rest of us.
favourite question is ..."going for coffee?"

In fact, his

Tim does not like keeners

so he can often be found sitting with Romanchuk and Pedenchuk in

their structural lab.

Tim's ambition is to continue his education

beyond the B.Sc. level and eventually become an employed geophysicist
or an unemployed geophysicist.

Igneous Petrology.

His favourite subject is, of course.

Tim never fails to become amazed over the electrical

properties of Tholelitic Basalts.

When asked about his thoughts of

the last four years, he said ... "let

'

s

go for coffee."

Tim's thesis topic is the study of the silver mines of the Mainland
Belt, in particular- the West Beaver Silver Mine.

The Silver belt is

under study at the present time to determine zonatlon of the veins
and mineralogical implications.

The relationship between the diabase

sills overlying the Rove argillites is a study of both academic and

economic interest.

�Keith Peden
Nickname :D ip ix Pedenchuck
Work Experience: Junior Assistant, (Basemetals)
Mattagami Lakes Mines, summer 1974
Underground Technician, Inco,
Shebandowan, Summer 1975
Expiditor, Imperial Oil, summer 1976
Great Lakes Timber, summer 1977
Thesis Topic: The Nature of the ShebandowanQuetico Boundary

Keith Peden, sp. Dipix Pedenchuck- This creature, native to the
Thunder Bay area, may be found in its natural state in and about the

Geology Department. It has been known to visciously attack cars, in
particular - Bugis Volkswagonis, by kicking various parts and leaving
said parts of this species scattered across the Thunder Bay region.

When not found in the hallowed halls of Lakehead University it may be
found scuba diving in the waters of Lake Superior or snowmobiling across
the countryside. Nocturnal activities include Geology socials, Ukranian da^ices and/or defiling parked vehicles (notably Plymouth Furylx)

This known instigator of practical jokes may be associated with its

neighbouring species - Stickus Romaninskl - in the structural lab. This
association, known in the scientific world as the Dipstick relation,
has been known to cause dlsasterous effects. A final word of caution,
this species may become violent when compared to a Cumberland Street

drunk.

The boundary between the Shebandowan-Wawa volcano-plu tonic belt
and the Quetico Gneiss belt has been taken by some to be a distinct

hiatus separating these two belts as being critically different subprovinces. Still others have suggested that the differences between
these two sub-provinces is superficial and that the boundary is a

gradational one. The purpose of this research is to objectively
observe a section of outcrops intersecting this boundary. Most of the

observations are based on mineralogy and metamorphic deformation.

V

�Bernie Schnieders
Nickname: Bruno
Work Experience: Oil Field Geologist, AtlanticRichf ield
Summer 1976, Alberta
Junior Assistant, Noranda
Summer 1977, N.W.T.
Thesis Topic: Determination of Volcanic Terrain;
Silicified Pillow Breccias or
Agglomerates

Bernie is one of the more talented members of our fourth year
class.

His travelling music show complete with guitar and banjo

have entertained everyone,

(except that particular French girl.)

Bernie has asperations of opening "Bernie'

s

soon as he makes enough money after graduation.

Tackle Shop" as
I

guess Bernie

wants to be a geologist at some time, as long as it doesn't
interfer with his fishing and hunting too much.

He has spent one

summer working for Noranda in the Northwest Territories, and it

sounds as if he had a real 'blast'.

If worse comes to worse,

I'm

sure he has great potential as a manager of an A&amp;P store.

Bernie is writing his thesis on some volcanic units he worked
on this summer in the Northwest Territories, trying to determine
if the fragments are silicified pillow breccias or agglomerates.

'Bruno' can hardly wait to graduate,

since all this school

'bullshit' interferes with his regular visits to the College

dances.

He'll probably never be quite the same after spending

the winter at the 'Pink Paradise', but
as bad as the 'Wiley Street' life.

I

guess its not quite

�Gord Turner
Nickname: Gink esq.
Work Experience: Geophysics and Junior Mapper
Um ex summer 197 6
Contract line cutting and staking
Winter 1976-77
Senior Mapper, Umex, summer 1977
Contract staking, winter 1977
Thesis Topic: A Comparative Study of the Genesis
Of a Massive Sulphide Showing,
Savant Lake
,

Gord is a member of the infamous Wiley Street Revue.

A site

of wide intoxicating parties, Gord is frequently seen leaving it

in less than perfect state in an attempt to make it to those 9:30

geochemistry classes.

As well as selling T-shirts, playing depart-

ment hockey, and extensive testing of local ski hills, Gord oc-

casionally is found working in the Mineral Deposits Laboratory.
Having his home in Brampton Ontario and working with UMEX for
2

summers he has travelled around considerably.

His future plans

include being a successful exploration geologist.

Cord's thesis topic is a detailed study of a massive sulphide

occurence

of the Copper -Lead-Zinc type located

Savant Lake Ontario.

7

miles north of

Research on the property includes geological

and geophysical interpretations and sampling for detailed geochemical

analysis.

Extensive mineralogical work with thin sections and

polished sections was also prepared.

The ultimate objective of the

research is to compare the genesis of this showing with the model
proposed by

Sangster in 1972 and to consider relationships with the

processes operative at Mattabi as described by Franklin in 1975.

V

�I

Roman Tykajlo
Nickname: Romulus Stickus
Work Experience: Junior Assistant, Noranda (Winnipeg)
Keewatin District, N.W.T., (Uranium)
Summer 1977
Thesis Topic: Strain Ellipsoid in Archean Conglomerates,
Shaba qua, Ontario

Roman is the better half of the Dipstick relationship, i.e.
the Stick, alias "Romulus Stickus".

Geology Department.

He is our token Ukranian in the

Roman can be found in his structural lab anal-

ysing the structures of the fairer sex passing in the hall.

He never

quits his work, even on tea breaks in the cafeteria he is still doing
his analysis.

When he is not busy studying structures, he can be

heard muttering "quel bummer" as he wades through his assignments.

His pet peeve is the Geology Year IV class since his lab is always
used for their discussion periods.

Although Roman is supposedly in

Geology he actually prefers Physics and hopes to emulate our favourite
Physics professor, John.

Roman hopes to eventually become a foreman

for GM.

Deformed conglomerates are useful in the study of strain in
that the sand and pebble sized clasts become homogeneously strained

from essentially an original ellipsoid to a final ellipsoid which is

markedly different from the original.
methods.

This can be done by several

The shape and orientation of the final ellipsoid can be

determined by measuring axial ratios and angular deflections of
major axes on three mutually perpendicular sections, then combining
this two dimensional information into a three dimensional model.

�Mark Wittrup
Nickname:Markus, Splash, The Incredible Hulk
Work Experience: Junior mapper, O.D.M., Atikokan, 1975
Junior mapper, O.D.M., Red Lake, 1976
Portage Crew, M.N.R., Quetico Park, 1977
Thesis Topic: Stromatolites of the Lower and Upper
Algal Cherts, Gunflint Formation

Mark grew up in the Inner City Slums of Toronto.

He first

became interested in geology by collecting Ordovician Trilobites
along the polluted beaches of that fair(?) city.

His big break

came after grade 13, he was accepted at Lakehead University after

considering a career in muffler manufacturing.

After working two

summers as an eunuch for O.D.M., he got his balls back (Ed's note,
footballs?) and took a job with the infamous Quetico Park portage

crew who motto is "The Noble Torture."

Presently he is trying to

avoid admittance into the L.U. Geology five year program and is

gainfully employed as a 'baby sitter' for K House in the L.U.
residence.
If asked about the future, he replies

that eventually he

would like to become a successful exploration geologist.

For

the immediate future however it will be one more summer in Quetico
and then return to L.U. for M.Sc.

Before he gets tied down to a

woman he wants to do a pubcrawl of Australia.

Commonly, Mark

can be heard saying such things as.... "Can we have another

round at this table?" and "Don't worry. I'll get it done...
eventually.

Mark's thesis is a pictorial documentation of the primitive

marine algal life forms in the Proterozoic sedimentary sequences
within the vicinity of Thunder Bay.

Hopefully this thesis will

provide someone with a basis with which to do more detailed work

on the stromatolitic environment and possibly the origins of
life on the earth during this period.

�Gordon Yule
Nickname: 'Gotts Dam'
Work Experience: Geophysical Operator, Noranda,
N.W. Ontario, Winter-Summer 1974
Junior-Senior Assistant, Noranda,
N.W. Ontario, (Uranium) Summer 1975
Contract Staking, Winter 1975
Junior-Senior Assistant, Noranda,
N.W. Ontario, (Basemetals) Summer 1976
Contract Staking, Winter 1976
Senior Mapper, Gulf Minerals,
N.W.T., N.W. Ontario, (Uranium) Summer 1977
Contract Staking, Winter 1977

This native of Longlac is a renowned O.K. used snowshoe salesman whose
territories extend from the balmy regions of Longlac to the barrens of the
Northwest Territories. When we cornered this man in the murky depths of
the Waverly Hotel,
(noted for its fine clientel) he recounted this tale
of the dreaded geologic plague known as "Marathon Madness";
"T'was way back in '76, when one of my associates
from Wiley St. said that we were gonna go on a
little class field trip to this here place called
Marathon on a real futile exercise. After seven days
and what seemed like forty nights the work had
just begun! We worked and griped, we sweated
and cursed, we complained and thought that our work
was in vain; after all, we weren't going back there again.
ha:

When the field season came in '77 I had all but
forgotten "Marathon Madness" and the curse that lay
on the place, but sure enough, the first job of
the season was in that dreaded place-"Marathon"
Well, all I can tell you is that the class trip
in '76 came in real handy. I figured there was a
moral in there someplace and it goes something
like this: "you can't believe all your Profs
all the time, but you've got to believe some of
the Profs some of the time."
Well, I kind of wondered about this guy and 1 decided to find out what
he'd been up to in the last few years, and this is what I came up with.
Well, it seems that he started out in this doomed profession in the winter
of '74 as a geophysical operator for a company called Noranda Exploration
and stuck it out for a full three field seasons and came out as a JuniorSenior Geologic Assistant in '76. When I met him in '77, he was working
for another company called Gulf Minerals Canada as a Senior Assistant
Geologist and had just finished a stint north of the Arctic Circle.
Seems this guy has worked in everything from base metals to uranium
using geologic and geophysical methods of prospecting. Last 1 heard of
him, he had just been certified as an honest to goodness PROSPECTOR
by the Prospector and Developers Association.

�rraii'^
Socials

�•

MusicaI MooSC5
M,^w logics

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�Geology Club Field Trip

�3rd Year Geology

100 years ago, disaster struck the Great Lakes Nickel Mine - 4 of
their exploration geologists were lost when the mucker they were working
on mysteriously plunged into the murky depths of the mine.
Pictured below after they reemerged this past year Rob Lucas,
A1 Schappert, Jim Rodgers and Rob Fnukal had little to say except....

"WE'RE HUNGRY!"

�Robert Fnukal
Work Experience: Junior Assistant, Mattagami Lakes Mines,
Ignace-Sturgeon Lake, KapuskasingTimmins, summer 1976
Junior Assistant, Mattagami Lakes Mines,
Longlac, Ignace-Sturgeon Lake, north of
Lake Nipigon, summer 1977

Jim Rogers
Work Experience: Labourer, Upper Lakes Shipping
Summer,

1973-77

Robert Lucas
Work Experience: Junior Assistant, Falconbridge Nickel,
Lake Nipigon Area (Uranium), summer 1977

Allan Schappert
Work Experience: University pollution and sediment
research, summer 1976
Seismic Technician, Energy, Mines and
Resources, Yellowknife, summer 1977

�Thank you, GORD TURNER

Vie

Do do

it

best

!

�UMEX
Bnloi Mifliere ixplirations and

A

Subsidiary

UNION
MINIERE

of

FIVE OFFICES

EXPLORATION
1935

DEVELOPMENT

Corperation

Minini

Leslie

lilted

Belgium

CANADA

IN

200-4299 Canada Way

Street

TORONTO
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(416)

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(604)437-9491

4105-1

Place

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Mane

MONTREAL

FINANCING

(514)

1068

-7e

VAL D'OR.
(819)

Rue
P.O.

824-2994

866-2461

2050

Blvd

St.

Cyril le

West

STE. FOY, QUEBEC
(418)

683-1939

LAKEHEAD UNIVERSITY GEOLOGY CLUB
snip ROCK IRON MINIS
Atikokan.Hiitario

IIMITIH

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"/

/

SILLMAN

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COMPANY (NORTHERN) LIMITED
GENERAL CONTRACTOR

555 Eighth Avenue, Box 2536, Thunder Bay, Ontario

PjB 3G1

Telephone {807) 344-8484 - Telex 073-4381

ARMCO

V

AUTHORIZED DEALER Atiiico BuildiiiE

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TONE LIMITED
as» FORT WILUAM ROAD. STATION

"R".

THUNDER BAY. ONTARIO • TELEPHONE

3AS-1A17

MANUrACTURKRS OP A COMPLtTt LlNM OP CONCPKTK MASONPY

�School

’76

�Join the Rest of the

Motor

Crest
Red

Crowd

River

MEMORIAL AVE. (HWY. 11B

DINING

ROOM

LIQUOR

-

Crest

Road and Junot

BUDGET
LUXURY
HOTEL

17B),

THUNDER BAY, ONTARIO, CANADA P7B 3Z5

&amp;
1

LOUNGE
1

Double Bed

2 Double Beds

Cots

Call

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at

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17.95

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•

3 per

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for children

•

4 per

26.95

under 13

Collect

(807) 344-5744

•H*

Circle

Inn

�Second year - One great big happy (?) familyl From left; Eugene Kent, Dr. Kehlenbeck,
(in front), John Scollie (in back), Murray McGill, Randy Farmer (in back), Ron Tweedie,
Joe Sipos, Mike Lucko, James Gresham (hidden), Tim Howson, Jack Parker, Dr. Mercy (in
back). Bill Palmer, Wayne Redditt, Heather Brown, Myra Gerow, and Bruce Jago.
Absent; Harold Kobler and Gonzalo Medina.

2nd

year
Sometimes the evening discussions
can get to you. They get to Jack
most of the time. Joe is just an
innocent bystander.

The essence of a good field trip Those evening discussions. Here we
see Wayne Redditt, Dr. Mitchell and
Eugene Kent "discussing".

1

�.

k

Heather Brown
Interests: Travelling, swimming, camping and
cross-country skiing. Heather was employed
by Noranda this summer

Randy Farmer
Interests: Fishing, hunting, field geology.

Myra Gerow
Interests: Playing squash, photography, travel
and car races. Myra worked for the O.D.M. for
the summer.

Tim Howson
Interests: Motorcycles and bartending.
Tim worked with the Ministry of Natural
Resources in Sault Ste. Marie this summer.

�Bruce Jago
Interests: Backwoods camping, antiques and field
geology. This summer Bruce worked for Noranda.

Eugene Kent
Interests: Cross-country skiing and photography.
Eugene worked for Falconbridge this summer.

Harold Kobler
Interests: Carpentry and circuit breakers.

Mike Lucko
Interests: Geophysics and his family; his wife
Edna, and their two sons, Randy and Eric.

�Gonzalo Medina
Interests: Getting his B.Sc. degree, judo,
fencing, and travel.

Murray McGill
Interests: Exploration geology, travelling,
photography and motorcycles. Murray was
employed by Dennison Mines for the summer

Jack Parker
Interests: "Even impaired walkers are picked up
by the police." From this quote we can easily
guess what Jack's main interests are. He was
employed by the O.D.M. for this summer's
work term.

Bill Palmer
Interests: Petroleum geology and paleontology,
ever since he was 5 years old. Bill was employed
by Falconbridge this summer.

�Wayne Redditt
Interests: Expensive stereo equipment and British
motorcycles

John Scollie
Interests: Photography

Joe Sipos
Interests: Igneous Petrology (so he says)

Ron Tweedie
Interests: Just your normal, basic, everyday healthy interests. We won’t enumerate
them.

�Scott Cheadle
Interests: Arch top banjo, snake handling,
nude kites, and Peruvian classic litterature
are his main interests. Marble classification
and dog paintings come in a close second.
Scott worked with some of the Profs at
Lakehead this summer

Mike Corey
Interests: Diving, cross-country skiing
and stamps. Mike worked for Falconbridge
this past summer.

Dan Malo
Interests: Scuba diving. Cross-country
skiing, winter and summer camping.

Scholarship Winners
From left to right; Heather Brown - J.P.
Bickell Bursary, Murray McGill - Abitibi
Paper Bursary, Bruce Jago - Bora Laskin
and C.P. Rail Scholarships, Myra Gerow C.P. Rail Scholarship, Mike Lucko - J.P.
Bickell Bursary.

�the

Lakehead University Geology Club
Wishes all Students a very Successful

Summer
Bruce Jago

,

locations
:
:
:

Gord Yule

President

69

3

Exploration Season

^cuuo*s (iouXracUw^
General Contractors

665

in

Asphalt, Concrete

Hewitson St., Thunder
Phone.. 623-1855

in

Thunder Bay

201 W. Arthur Street

853 Red River Road
1200 Memorial Avenue

Bay, Ontario

&amp;

Precast

P7B 5V5

,

Vice - President

(thunder bay)

ltd.

�PHILLIPS WILSON
,

LAND

ONTARIO

10-6A SOUTH

AND MILTON

LTD.

SURVEYORS

COURT STREET

THUNDER

BAY, “P” ONTARIO

345-0574

Telephone

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MIDW€^T

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1100

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THUNDER

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BAY.

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opportunity to extend

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REGINA

SASKATOON

PARTS

1

•

SALES

•

SERVICE

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film agents for

^

1

lakehead

university

PRISMATIC PHOTO
344-3791

�1

St

Year

First Year Geology Majors: Front row (left to right); Rick Dutka, Barry Rabishaw,
Burns Cheadle, Nick Spence, Rock Rice, George Chomacki, John Pearson, Scott Bruce.
Middle row (left to right); Rob Bennett, Mark Stevens, Brett Barnes, Rick Kemp,
Back row (left to right); Denis Samayou, Eric Albrechtsons,
Paul Gertzbein, Bill Love.
Missing; Sherri Baker, Warren Clendining, Dave Crocker,
John Etches, Blair Kite.
Rhys Denmore, Andrew Clarke, Ron Kumar.

���Message from the Geology Club
As president of this year's Geology Club I would like to express my
thanks to those people who made this year a successful one. Our club
executive was as follows: Bruce Jago, Club President; Gord Yule, Vice
President; Rob Bennett, Secretary-Treasurer, Geology Club and Yearbook;
Heather Brown, Social Co-ordinator; and Allan Schappert, Field Trip Coordinator. Without these interested people we would have only been a
name for LUSU to push around.
Instead they had to deal with people who
had an objective in mind and were determined to see it to its completion.

Because of our restricted budget we were in a delicate position as
far as funding was concerned, as well, the Student Union in all their
wisdom feels it is necessary to keep their various clubs in the dark concerning field trips and general LUSU policy. Consequently we could only
offer field trips to Silver Islet, the Silver Mountain area and an overnight excursion to Geco. Next year however, now that we the executive
have gained valuable operational experience, we hope to be able to expand
the activities of the club.

This year the club expanded in a different direction and a small group
of individuals decided that the Lakehead University Geology Department
should be represented once again in pictorial fashion within the pages of
The idea was conceived over a cup of coffee in the
a Department Yearbook.
Geology Club office while looking over the files of previous years. After
little discussion it was decided to go ahead. As this yearbook was a new
experience for those who put it together, we had a lot to learn and a lot
I can see now why more people did not feel inof mistakes to overcome.
clined to get involved.

As Editor of the yearbook I would like to thank those brave Individuals
who undertook this seemingly easy task and who have found time to see it
to its culmination.
In particular, I would like to thank Heather Brown
my Co-editor, Myra Gerow my right hand assistant, Murray McGill photo manager, Rob Fnukal advertising manager, Rob Bennett and Mike Lucko sales
managers, Mark Wittrup who did custom developing for us as well as cartoons
and a host of other people. I would like especially to thank Sam Spivak
who relentlessly made headings and advertising layouts for us and who put
up with our incessant bothering.
This yearbook would not have been possible
if it had not been for these people, THANKS AGAINl

Yours truly.

Bruce Jago
President, Lakehead University Geology Club
Editor, Geology Club Yearbook

�IN

MEMORIAM

Jack

J.

Clue

1950-1978

received his B.A. degree in Geography in 1972 and his
Honours B.Sc. degree in Geology in 1975. After graduation from
Lakehead University he joined the Manitoba Department of

Jack

Natural Resources as a geologist.

work

His future plans for graduate

geology were prematurely halted by his untimely and
unexpected death in late January 1978.
in

The members of the Geology and Geography departments
expressing their sympathy to his family and friends.

join in

��.

V

����</text>
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                    <text>����GEOtOOY JOURflM
1979-80

th

5

CDITIOn

�b.cKeod)

�Dedication

JULIAN

GIFFORD

CROSS

1888-1972
The diamond drill, perched on the ice of Steep Rock Lake in Northwestern
Ontario, chugged away, the sound of its steam engine muffled by the snow.
The
driller called to a man who was sitting in a corner of the drill shack writing
in a notebook.
The man picked up some of the sludge, looked at the dark brown
specks for a moment, and then quietly said, "Well, that's just worth a million
dollars to me!"

Julian Gifford Cross probably had reason, that March day in 1938, to be
much more excited than he appeared to be. The hematite fragments that he held
in his hands were the first proof that iron ore lay under the waters of Steep
Rock Lake. He must have felt a tremendous sense of satisfaction at that moment
in knowing that his theory, developed ten years before had been proved correct.
In spite of the set-backs, disappointments, and skepticism from his colleagues,
he had stuck stubbornly to his conviction that iron ore lay beneath Steep Rock
Lake.

The Steep Rock iron ore deposit was not the only major discovery made by
Julian Cross. In the late 1920' s, Julian and his brother John staked claims at
It was on these claims that they
Shebandowan Lake in Northwestern Ontario.
discovered the Shebandowan nickel deposit. In the early 1930' s, INCO purchased
the claims from the Cross brothers for $250,000 and, a good portion of this
amount became the seed money for the start of exploration at Steep Rock Lake.

Those who knew Julian Cross, when asked to describe him, invariably used
For the man who
words like "quiet", "tenacious", "persistent", and "kindly".
was the discoverer of two major orebodies he was completely unspoiled. He is
and a remarkably
best known, and probably happiest as a prospector
successful one
with a packsack on his back, and a prospector's pick in his hand.

—

—

—

Taylor, B., 1978, Steep Rock
The Men and the Mines
Quetico Publishing, Atikokan Ontario, 144p.

�YOUR
UNIVERSITY
Serving

Northwestern
Ontario
since 1965
.

.

.

Offers comprehensive programs in Arts,
Business, Education, Engineering, Forestry,

Library Technology, Nursing, Outdoor
Recreation, Physical Education, Science.

Provides instruction on-campus and off,
part-time and full-time, fall, winter and

summer.

Has athletic and recreational facilities
including an Olympic swimming pool, squash
courts, gymnasia, tennis courts,

comprehensive varsity and intramural sports
programs.

Has an

program
development and for special

active continuing education

for professional

groups.

Keep

in

touch with us through the

Department of Alumni
Lakehead University,
Thunder Bay, Ontario.

Affairs,

�Message from the President

On behalf of my colleagues,

I

would like to take

THIS OPPORTUNITY TO EXTEND MY CONGRATULATIONS TO THIS YEAR'S

GEOLOGY GRADUATES, AND TO WISH YOU WELL

IN

YOUR FUTURE

ENDEAVOURS.

Lakehead University's geology program

is

recognized

AS ONE OF THE FINEST IN THE PROVINCE AND YOUR DEGREE WILL

STAND YOU IN GOOD STEAD IN THE EVER-EXPANDING FIELDS OF
GEOLOGY, ENERGY AND FUEL DEVELOPMENT.

Once again, good luckj and keep in touch with your

UNIVERSITY.

G.A.

Harrower

President.

�Compliments of the

Faculty of Science

Lakehead University

�Message from the

Dean of Science

Once again it is my pleasure to compliment the

Editor and Staff of the Geology Yearbook for covering a very

important aspect of student life at Lakehead University.

Yearbook is

a

The

permanent record of the academic, professional

and social activities of students majoring in Geology at

Lakehead University.

I

note that it is one of two yearbooks

published at the discipline level at Lakehead University.
I

wish those students who contributed to this yearbook my best

in taking part in this very worthy venture.

Yours sincerely.

Dean
Faculty of Science

��Message from the Chairman

It

PRIDE THAT

I

is

with great pleasure and a measure of

CONGRATULATE THE EDITORIAL BOARD AND THE

MANY CONTRIBUTORS WHO MADE THIS ACCOUNT OF STUDENT

ACTIVITY A SUCCESS.
Your group has shown their abilities to

UNDERTAKE A MAJOR TASK AND CARRY IT TO A SUCCESSFUL

COMPLETION EVEN THOUGH NUMEROUS OBSTACLES HAD TO BE
OVERCOME ALONG THE WAY AND THE ROAD WAS NOT ALWAYS
SMOOTH.
In

the not to distant future you will embark

ON YOUR CHOSEN CAREER AS A GEOLOGIST.

It

IS

OUR HOPE

THAT YOU WILL BE SUCCESSFUL IN YOUR PROFESSION AND THAT
THE EDUCATIONAL EXPERIENCES AND FRIENDSHIPS YOU NOW

ENJOY WILL CONTINUE TO SERVE YOU WELL IN LATER LIFE.

Chairman

�CONGRATULATIONS AND
to the

M. W.

BARTLEY

WISHES

BEST

Graduates

&amp;

ASSOCIATES

LTD.

Geologists

209

Winnipeg Avenue

Thunder Bay, Ontario

the

Lakehead University Geology Club
Wishes all Students a very Successful

Summer
Rob Bennett

,

Exploration Season

President

John

* Join the Rest of the

Crest
Red

Crowd

Motor

River

at

Pearson Vice - President
,

the

Hotel

Road and Junot

Crest

&gt;y

��Dr. John Sydney Mothersill

,

B.Sc.
B.Sc.

(Physics,
Mathematics)
(Geological
Engineering)

Ph.D.

Background
Exploration Geologist for Standard Oil (N.J.)
Senior Geologist for Mobil International Oil Co.
Exploring for petroleum in Turkey, Nigeria,
France and Colombia, 1956-64
Associate Professor, Lakehead University 1966-78
Professor, Lakehead University 1978-present
Dean of Science at Lakehead 1975-present

The primary areas of research in which

I

have been involved during

the past several years are late-Quaternary paleomagnetic studies and sediment-

ologic studies.

The paleomagnetic studies consist of determining the late-

Quaternary paleo-declination

,

paleo-inclination, paleo-susceptibility and

paleo-magnetic intensity columns for northern Lake Superior for time parallel

correlation purposes.

This study has been extended into eastern Lake Superior

and Lake Huron to provide a time parallel correlation grid for the Great Lakes.
In addition,

the natural remanent magnetic direction will be used to determine

the virtual geomagnetic path for the late-Quaternary.

The sedimentological studies were centred around the Batchawana Bay

area and emphasize the use of grain size parameters as determined by the method
of moments to discriminate environment and sub -environment processes.

The

Batchawana area, which comprises a number of sedimentological environments,
will be used as a model for the post-glacial sediments exposed along the eastern part of Lake Superior and for the deep-water lakes in general.

�Dr. Edward Mercy , B.Sc., Ph.D., D.I.C.

Background
Lecturer in Geology, Imperial College of Science
and Technology, London, England
Lecturer in Geology, later Senior Lecturer in
Edinburgh, Scotland
Geology, University of
Professor of Geology and Chairman of the
Department, Lakehead University 1967-76
Professor of Geology at Lakehead 1976-present

Most of the existing textbooks of geochemistry
are disappointing to anyone who has a real
interest in the subject matter.
They are
disappointing because, in attempting to be
comprehensive, they trivialize the subject.
There are serious economic constraints on the size and cost of a publication
intended primarily for the university student market.
Comprehensiveness flies
out the window and the house is occupied by a poor half-starved creature masquerading as geochemistry. The falsity of his pose is compounded by hie declaration
that parts of mineralogy and petrology may be offered as substantial fare for
those who hunger after knowledge.
The essence of this purveyor of mis-inf ormation
is his belief that he knows about that which
he writes and that all that he writes
is all that is needful to know.
That he does it deliberately can hardly be
maintained. That he does it at all must be because he knows no better.

A serious critic ought to be prepared to redress the iniquities he discovers
in others even though in doing so he may impose upon himself a task of some considerable magnitude. Naturally, having made the decision to play the role of
creator rather than critic, he then seeks to place limitations on the nature and
extent of his dissertation so that the result may have a defined purpose. Despite
the gross enlargement and mis-use of the term in recent years, geochemistry is
properly concerned with the distribution of the chemical elements in Earth and is,
in this proper connotation, a fascinating subject of study with important, and
sometimes critical, implications for the general scientific understanding of
our planet.
There are three limitations on the scope of the proposed textbook which
provide the essential framework within which the principles of geochemistry
may be established. The first is that the overall chemical composition of Earth
and the manner of its formation and rapid evolution into a heterogeneous body
must be assumed on the basis of the extensive knowledge provided by astronomers,
meteoriticists and geophysicists. The second is that the accessible igneous
rocks of Earth's crust, knowledge of these being provided by mineralogists and
petrologists are suitable objects of study for the provision of the necessary
geochemical data. The third is that the writer and the reader have a sufficiently
wide and detailed knowledge of geology and chemistry that the discovery and
illumination of principles takes place without laborius, tedious and repititious
explanation
,

,

Given these parameters and provided that the focus of attention is firmly
fixed on the behaviour of the elements, then a textbook can be constructed.
Whether it has any principles - the author assumes as a philosophy that principles
do exist to be discovered and explained - is for the reader to decide.

�Dr. Manfred M. Kehlenbeck, B.A.

,

M.S., Ph.D.

Background
Visiting Professor, University of New Brunswick
1969-70
Teaching Fellow, Queen's University 1970-71
Assistant Professor, Lakehead University 1971-76
Associate Professor and Chairman of the Geology
Department, Lakehead University 1976-present

This past field season

began in late April

with the field school trip down the not-toosunny shore of Lake Superior.

Attempts to

reach the Ely greenstone belt and the Soudan
iron formation were unsuccessful, and our two vans had to beat a hasty retreat
from what rapidly became a winter wonderland.

From late May to the end of June, Warren Clendining and

I

crossed many a

farmer's field around Lappe in search of cleavages, graded-beds and pillows with
the hope that all these would somehow merge into a coherent story of structure

and stratigraphy.

It appears that our efforts were not in vain.

In late June

the sun finally decided to let summer enter Northwestern Ontario.

After some very

hot and dusty days, we packed up, and along with a rather questionable vessel

known simply as "Rubber Dingy", moved north to Dog Lake.
secured

Pleasant quarters were

at the Dog Lake Resort and work proceeded at full speed on the East Bay.

After a month on the water, it was time for me to move again.
place than the Alps to provide variations in elevation?

What better

It was rewarding to

observe on a grand scale some of the geological structures of this relatively
young mountain belt.

It was especially exciting to realize that I had been work-

ing in the Archean terrains in which the remnants of very similar structures

also occured.

The several glaciers which had to be traversed provided a fitting con-

clusion to my field season which had begun and was now ending with- SNOW.

�Dr. M.W. Bartley, M.Sc., Ph.D.

Background
Lecturer, University of Toronto 1938-40
Iron Ore Exploration since 1938
Steep Rock Iron Mines development 1940-48
Principal, Lakehead Technical Institute
1948-52
Honorary Professor, Lakehead University
1971-present
President of The Canadian Institute of
Mining and Metallurgy 1976

My primary interest is economic geology which embraces many sub-disciplines
including exploration, evaluation, development, and utilization as applied to
mineral deposits. This entails not only a knowledge of basic geology and mineralogy
but also an appreciation of the fundamentals of mining engineering, metallurgy,
economics, and management.
In the rapidly changing world of science and technology, specialization is
increasing, unfortunately, to the point where the traditional economic geologists
are fast becoming an endangered species.
This is regrettable but the trend can
be reversed.

The reversal can be accomplished by informal research consisting of planned
reading of journals in which case histories and techniques are described, by
attendance at meetings of earth scientists with similar interests, and plain old
If I am permitted to extend only one piece of
"bull sessions" with one's peers.
advice to budding economic geologists, it is to read, listen and ask questions.
I strongly recommend that all prospective geologists become members of and
take active part in professional associations.
It is through these affiliations
you can more easily broaden your education, gain professional stature, and
enhance lasting personal satisfaction.

My involvement in the mineral industry as an employee, as a consultant, and
been pleasant and rewarding. A highlight
was the realization that my education has never stopped.
to a limited degree as an academic, has

I wish you success, satisfaction, and many years of productive life after
graduation.

�Dr. Roger H. Mitchell, B.Sc., M.Sc., Ph.D.

Background
Lecturer in Isotope Geochemistry, University
of Oslo, Norway 1971-72
Assistant Professor, Lakehead University 1972-76
Associate Professor, Lakehead University 1976-present

Since the publication of the last Geology Journal, I have been on sabbatical
leave in Australia and reflecting on the fact that being a geologist presents one
with unrivalled opportunities for travel and the possibility of visiting places
the casual tourist would never stumble upon - places such as the Spinifex Inn Disco
in the Western Desert, the Orroroo Railway Hotel or Noonkanbah Tank No. 5.
Visiting such "places" enables one to obtain a feeling for a country which is not
available to the short-term visitor. Consequently, those of you who have doubts
about your chosen profession, whilst learning the ontogeny of graptolites or
standing amidst the black flies on a swampy greenstone belt, remember that being
a geologist will enable you to combine travel with a stimulating occupation if
you take advantage of the many employment options open to you.

Whilst in Australia, I found that the public generally respected geologists
and were aware of the nature of their work, presumably as a consequence of many of
Life for the
the towns having their origins as exploration bases or mine sites.
geologist in the field is, compared to Canada, relatively pleasant; a warm (to
very hot) and dry climate (unless you are in the monsoon areas) plus the ability
to drive almost anywhere - no muskeg, few trees, no portages, no second-growth!
,

The bulk of my sabbatical leave was spent irradiating myself at the University of Melbourne where I obtained new insights into the geochemistry of gold,
I also saw numerous recent volcanic
iridium and palladium in garnet lherzolites.
rocks, studied the art of chronomancy (or fission track geochronology), and gained
some familiarity with Australian painting.

Ed. note:

Dr. Mitchell was made a Professor in February of 1980.

V

�Dr. R. Garth Platt

,

B.Sc., Ph.D.

Background
Visiting Professor, University of Copenhagen,
Denmark 1969-70
NRC Postdoctoral Fellow, University of
Western Ontario 1970-71
N.E.R.C. Research Fellow and Staff Member,
University of Edinburgh, Scotland 1971-74
Assistant Professor, Lakehead University 1974-78
Associate Professor, Lakehead University 1978-present

So it is now two years since my last contribution
to the Geology Journal.
If I recall, the last
communication ended with the safe completion of
a nephelinite , basanite, phonolite hunt to Bathurst Island, N.W.T.
Subsequent work
has shown that the hunt was a success.
The bonus of discovering the first
occurrence of olivine melilitite in Canada merely added icing to the cake. These
continental rift valley volcanics are presently the object of geochemical, petrological
and mineralogical studies.
The first results will be discussed at a field workshop
on volcanism in rift and intraplate environments in July 1979 during a field trip
concerned with the alkaline vulcanism associated with Cenozoic stretching in

Western Europe.
The main research thrust has continued to be the Coldwell Alkaline Complex,
a location dear to the heart of many a Geology major from Lakehead.
What greater
delight is there than the Pic Disco, the Everest Hotel, the Red Dog dining-room,
Red Sucker Cove and Ministry girls from Neys Provincial Park? Recent work has
centered on the Nepheline Syenites and the numerous dikes intersecting the intrusion.
Currently M. McGill and B. Jago are completing a detailed study of the Southwestern
margin of the intrusion for their honours theses. This large alkaline complex will
continue to be the source of many challenging theses in the years to come.

Evidence is slowly emerging on the presence of past carbonate-rich magmatic
activity just to the west of the Coldwell Complex. The McKellar Harbour region
is the locus of numerous C0 2 -rich, K^O-rich ultrabasic lamprophyres which could
easily be mistaken for kimberlites (Diamonds!) but which are most likely related
to carbonatites
These dikes contain varying proportions of olivine, phlogopite,
calcite, apatite, spinel, perovskite and melilite and one contains significant
amounts of a very rare Zr-rich, Ti-rich andraditic garnet. As of now only four
These dikes are believed to
localities in the world are known for this mineral.
be associated with the activity responsible for the formation of the Prairie Lake
Carbonatite lying some 35 kilometres to the north of McKellar Harbour.
.

So much for now, so until the next time, to all geology majors, good luck
and may the spirit of igneous petrology be with you.

�Dr. Stephen A. Kissin , B.Sc., M.S., Ph.D.

Background
Postdoctoral Fellow, McMaster University 1973
N.R.C. Postdoctoral Fellow, CANMET, Department
of Energy, Mines and Resources, Ottawa 1974-75
Assistant Professor, Lakehead University 1975-79
Associate Professor, Lakehead University 1979-present

My research activities over the past year and
summer, in particular, have been varied and
quite interesting.
I placed my work on tin-bearing sulphides on the back burner
for a while, having reached several impasses on that subject.
My efforts since
then have been concentrated on some new projects.
After completion of my work pertaining to spring term and field school in
1979, I spent a few weeks readying a paper for publication.
This was followed by
the frantic preparation of an abstract for the Meteoritical Society meeting which
was held later in the summer. My next project was a jaunt into the field with
M. Lucko to examine pegmatites in and around the Quetico Belt along Highway 527.
We observed numerous pegmatites, one moose, and experienced the coldest June
weather to my recollection. There were, however, essentially no bugs!
In early July, I took my wife and two small children to the Los Angeles area.
did nothing geological except to attempt to find the San Andreas Fault as we
flew over it.
I returned home impoverished and in need of another holiday.
Unfortunately this was not forthcoming, and I found myself readying my paper for
the Meteoritical Society.
In doing so I happened to learn that Dr. Borradaile
was editing a book.
I volunteered a contribution on shock structures in iron
meteorites. My meteorite work dealt with the sulphide mineralogy in one of the
chemical groups of iron meteorites and the various implications one could make
from such studies. Although much of my data had been collected some time ago, I
found some gaps which necessitated a one week visit to the University of Toronto
to use their electron microprobe.
I

As a guest of the University I was allowed to stay in the Medieval splendour
of Hart House, where my room was furnished with antique French Canadian furniture
complete with original paintings by Sir Frederick Banting. My probing work went
quite well and for once, I was able to do some additional work on silver -mercury
minerals from the Stanley area west of Thunder Bay and, on indium-bearing

sulphides from New Brunswick.

Upon my return to Thunder Bay a few weeks were spent preparing my paper on
iron meteorites and, in the last week of August, I left for Germany where the
Meteoritical Society was meeting. I spent a week on my own in Southwestern Germany
and a week in Heidelberg attending the meeting.
My presentation was well received,
and I was satisfied that the trip had been worthwhile from the standpoints of both
business and pleasure. I returned to Thunder Bay thirty-six hours before the
start of classes.

�Dr. Roy J.

Shegelski

,

H.B.Sc., M.S., Ph.D.

Background
University of Toronto 1973-77
Lecturer at Lakehead University 1976-78
Assistant Professor, Lakehead University 1978-present

I

am pleased that the Geology Club is continuing the yearbook and

wish them the best of luck in their endeavours.
I

have been investigating strata in Northwestern Ontario for the past

summer and have experienced both success and failure.

The field conditions

around Thunder Bay are pleasant; pollution keeps the fly population down,

tourist-ridden parks provide well worn pathways to outcrops, and the beautiful
scenery along the Current River is enhanced by bikini-clad beauties which
proved to be a major distraction to section measuring by assistant B. Cheadle
and myself.

What was that thickness now?

The field season ended with a bang

some 40 miles east of Pickle Lake on Lake St. Joseph as B. Berger and myself

surfed over a submarine drumlin and lost propulsion in our motor.
came three days later aided by a "Sportsman's Survival Flare".
this misadventure, research sampling and field trips continued.

which

I

Air rescue

Undaunted by
The message

have based on this summer's experience is that field geology is al-

ways a mixture of hardship and triumph, but the necessary element which makes
it feasible is perseverance.

�Dr. Graham Borradaile , B.Sc., Ph.D.

Background
Senior Demonstrator in Geology, Durham
University, U.K. 1970-73
Assistant Professor in Geology, University
of Amsterdam 1973-78
Assistant Professor, Lakehead University 1978-present

Ed. note:
Dr. Borradaile was made an Associate
Professor in February of 1980.

My family and

I

came to Thunder Bay for the

beginning of the school year in 1978, after having
lived and worked in Amsterdam for the previous five years

We have now settled in the bush just outside of town and, according to the time of
year, we greatly enjoy chopping wood, skiing, attempting to canoe and digging snow.

After a hectic first year translating and paraphrasing my Dutch teaching notes
(which hopefully helped the class!),

Together with Dr. Kehlenbeck

I

I

was able to enjoy my first Canadian summer.

collected data on metamorphism from the shores of Dog

Lake (excellent for surfing but awful for boatlanding)

,

and

I

have also been

researching into "fault rocks" (mylonites, pseudotachylite, cataclasite,

...etc).

The fault rocks occur in several belts, each perhaps a kilometre wide and hundreds
of kilometres long, in the shield of N.W. Ontario.

The most spectacular example, the

Quetico "fault", just north of the city has been the focus of my attention.

I

have

pursued other more theoretical research, partly using recently acquired data,

concerning changes in temperature distribution with time in metamorphic belts and

grain-boundary sliding in metamorphic rocks.
I

much enjoyed working with Howard Poulsen and Myra Kennedy on their respective

metamorphic/structural research topics last summer.

I

also greatly profited from their

help in sampling, looking at the local geology and in thinking about geology in general.
I

hope that those of you who will be graduating and leaving LU this session

will carry equally pleasant memories of 1978-79 and that you never forget all your
sunny, blue-skied student days at Lakehead.

�K.H.

(Howard) Poulsen , B.Sc.
B.Sc.

(Physics)
(Geology)

Background
Exploration Geophysics 1961-71
High School Teacher 1968-69
Research Assistant for J.M. Franklin 1972-75
Senior Technician and Faculty Assistant,
Lakehead University 1975-present

In addition to my full-time duties as departmental hockey convener and as
Hoots’ official interpreter, part of the past year has been spent maintaining and

supervising the geochemistry laboratory.

The initiation of the graduate program has

seen a renewed demand for geochemical analyses performed both by myself and graduate
students.

Our whole rock and trace element analytical programme, while centered in

our own laboratory, relies heavily on apparatus housed in the Science Instrumentation

Laboratory which is maintained by Dr

.

T. Griffith and his staff.

Our students are

very fortunate to gain hands-on experience in this facility on equipment that

actually works!

Aside from the above departmental responsibilities, the past year has been
occupied with my continuing research interest, the Precambrian geology of the Rainy

Lake region.

Of particular interest to me was a workshop on the geology of the

International Boundary held at Fort Frances in May 1979.

Valuable discussions were

held with officers of the Geological Survey of Canada, the U.S. Geological Survey,
the Ontario Geological Survey, the Minnesota Department of Natural Resources and

university representatives.
numerous outcrops.

Seminar presentations were followed by visitation to

It might be pointed out that the most memorable exposures were

seen at an establishment known as "Nick's Zoo" where the role of fluids in geology

was heartily discussed.

Unfortunately

I

failed to record the attitudes of minor

structures in my notebook so that stereographic representation of the results is
not possible.

�Ronald Bennett
Ron is the "guiding light", the "shepherd"
if you will, within our geology department.
For
friendly advice or a good ol’ Scottish yarn, Ron's
the man to see!
He was the Chief Laboratory Technician at the
Grant Institute of Geology, University of Edinburgh,
Scotland from 1936 to 1967.
In 1967 he joined the
Geology Department staff at Lakehead and, as our

principal technician, he does specialized work
related to faculty research projects.
Outside of the university Ron is an active
participant in Kaministiquia community functions.
He is an avid fisherman and carpenter, and enjoys
putting his homebuilt sauna to good use.

Sam Spivak - Chief Draftsman
Principal Technician
Map Librarian
The majority of my working hours (in this
second decade as an employee of this fine
establishment) are spent preparing maps, diagrams,
teaching aids and special displays as well as a
substantial number of illustrations for research
publications. A fair amount of time is spent in
the maintaining of and cataloguing of new
acquisitions to our map library.
A regional seminar on "cartographic techniques"
was held at Sir Sanford Fleming College early in
I was fortunate to have attended this seminar
1979.
for the purpose of acquainting myself with some of
the new ideas for, and methods of, map production.
My extra curricular activities within the
university include organizing and participating in
the annual student-faculty-staff hockey games as
well as being an active participant on the squash
courts

�Ain Raitsakas
Ain was born in England, but was fortunate
enough to have emigrated to Canada at an early
enough age to avoid the obviously deleterious
effects of such a birthright.
He was educated
at the University of Waterloo and at Lakehead
University
Since 1973 Ain has been associated with
the Geology Department through his work with
the federally supported Seismographic Station
at Lakehead, lending a prestige and sophistication
to the department that is uncommon in such an
earthbound discipline.

Bill Mcllwaine
Bill was born in Toronto and received
his early education there.
His high school
and university educations were obtained in
England and at the University of New

Brunswick respectively. After spending
fifteen years working in the bush, ten of
them as a field geologist with the Ontario
Government, he decided that more of his
time should be spent at home.
With this in mind. Bill joined the
Geology Department staff at Lakehead in
1978.
As a lab technician much of his
time is spent at the grind in the geology
lab in the basement of the Centennial
Building.
It is here that all of the
departmental thin sections for teaching
and research are prepared.

�.

Illlllllllllllllllllllllllllllllllllllllllllllllllllllllllll

THE DEAN:
-leaps

tall

buildings

in a

single

bound

more powerful than

a locomotive
-is faster than a speeding bullet
-is

-walks on water
-gives policy to

God

THE DEPARTMENT CHAIRMAN:
single

bound

powerful than a switch
-is
just as fast as a speeding
walks on water if the sea is calm
-talks with God

engine

short

-leaps

buildings

a

in

more

-is

bullet

PROFESSOR:
-leaps short buildings with a running start and

favourable winds
almost as powerful as a switch engine
-is faster than a speeding BB
-walks on water in an indoor swimming pool
-talks with God if special request is approved
-is

ASSOCIATE PROFESSOR:
-barely clears a quonset hut
-loses a tug-of-war with a locomotive

-can

fire a

speeding bullet

-swims well
-is

occasionally addressed by

God

ASSISTANT PROFESSOR:
-makes high marks on walls when

trying to leap
buildings
-is run over by locomotives
-can handle gun without inflicting self-injury
-treads water
-talks to

Wendy Bons

animals

INSTRUCTOR
-climbs the walls continually
-rides the rails
-plays Russian Roulette
-walks on thin ice
-prays a lot

GRADUATE STUDENT:
-runs into tall buildings
-recognizes locomotives two out of three times
-is not issued ammunition
-can stay afloat with a life jacket
-talksto walls

Wendy is originally from the Toronto
area where she received her high school and
college education.
She has spent the past
five years in Thunder Bay, the last two and
a
half years spent in the Geology Department
as Departmental Secretary.
Duties in the
department include such things as typing,
filing, handling of incoming and outgoing
calls, departmental budget documentation,
documentation of faculty N.R.C. grants, and
generally keeping things in line.

UNDERGRADUATE STUDENT:
over doorstep when trying to enter buildings
-says "Look at the choo-choo"
-falls

-wets

self

-plays in

with a water pistol
puddles

mud

-mumbles

to self

DEPARTMENT SECRETARY:
-lifts tall

buildings and walks under

them

-kicks locomotives off the track
-catches speeding bullets in teeth and eats them
-freezes water with a single glance
-IS

GOD

lllllllllllllllllllllllllllllllllllllllllllllllllllllllllllf

Judy Vogrig
Judy is from the Thunder Bay area and has
had the pleasure of working for Dr. Mothersill
Her job is to
for the past year and a half.
try and keep a busy office running as smoothly
as possible so that the Dean can accommodate
all the important and pressing items that
confront him both administratively and
academically

��Riocanex
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��.

Ben Berger
I graduated with an H.B.Sc. Geology degree from McMaster
University in 1975. Between 1975 and 1978 I worked for
Noranda Exploration and was based out of their Thunder Bay
office.
I spent the summers of 1978-79 working for Selco
Mining Corporation in the Thunder Bay area, Ontario and the
Kamloops area, B.C. respectively. My employment with Selco
and Noranda has provided me with mapping, geochemistry, and
geophysics experience in both base metals and uranium exploration.
In 1978 I enrolled in the M.Sc. program at Lakehead
University. My thesis work involves the compilation of volcanic
and sedimentary stratigraphy in the Lake St. Joseph area of
Northwestern Ontario.
My second year of studies at Lakehead has been enlightened
by the fun and games to be had with the third year class while
trying to teach them ore petrology and the finer points of
"Crest-manship"

John Mason
For the
I graduated from Lakehead University in 1975.
last five years I have been employed with the Ontario
Geological Survey (formerly the Ontario Division of Mines),
Ministry of Natural Resources, Thunder Bay as Geologist
Assistant and presently as Resource Geologist. The Thunder
Bay office of OGS is responsible for an area from White
River in the east to Atikokan in the west and north to the
54th parallel.
My M.Sc. thesis concerns the Archean stratigraphy of
Precambrian
the Kaministiquia Area west of Thunder Bay.
stratigraphy and economic geology are my main fields of interest.

�Scott Cheadle
I completed my H.B.Sc. in Geology at Lakehead University
following two years in the Department of Geophysics and Astronomy
My summer work experience has included mapping with
at U.B.C.
Dr. Kehlenbeck, a short term as the seismic technician under Dr.
Mothersill, and two summers as a general research assistant to
The topic of my H.B.Sc. thesis was
Dr. Mitchell and Dr. Platt.
a magnetic mapping and modelling of the Barnum Lake Pluton, and
it was completed under the supervision of Dr. Kehlenbeck.
As part of the M.Sc. program, my work in the Barnum Lake
area is continuing to include a broader magnetic and gravimetric
survey of the area and a more detailed modelling attempt at the
My
three dimensional configuration of the structures present.
principal interests in geology are crustal evolution and Archean
Tectonics. Outside of geology, my interests include skiing,
hiking, cameras, certain fretted instruments, the Rockies and
Export Ale during numerous evenings in front of televised football.

Doug Lehto
In leafing through past editions of the Geology Journal,
notice that it provides most people with an opportunity to
summarize their most recent activities in geology.
Since my
summer activities in 1979 can be summed up in terms of building
a "home" in Thunder Bay, I will begin my geologically related
tale from the time of my graduation from Lakehead University.
After graduating in the spring of 1975, I joined the staff
of the Geology Division, Saskatchewan Research Council,
Saskatoon, and worked with them until April of 1979.
I consider
myself fortunate to have arrived in Saskatchewan at the "dawn"
of the latest rush in uranium exploration.
During the summer
of 1975 I became involved in a geochemical study at the Duddridge
Lake uranium discovery.
It certainly was a new experience for
me having previously worked in base metal exploration in Ontario
and having left Lakehead with a thesis on structural geology
fresh in my mind. How quickly one adapts!
I later became
involved in other multi-media geochemical projects and, it was
during this period that my interests were directed towards lake
sediment geochemistry.
And so I find myself back at Lakehead as a graduate student
doing research in lake sediment geochemistry. My current
research involves an investigation of uranium partitioning in
recent lake, stream, and bog sediments from Northern Saskatchewan.
I

�&lt;

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�Graduands

�.

Heather Brown

Heather has the distinction of being Geology IV s only
single female. The question of her availability, however, will
have to be taken up with John.
She is a diligent worker, but
always has time for a smile for everyone.
Heather enjoys outdoor activities, especially snowshoeing,
cross-country skiing, and geophysics!?! Swimming and reading
are other favourite pastimes. Heather's organizational skills
were evident from the excellent socials she planned as social
coordinator for the Geology Club for 3 years.
Heather has gained much valuable experience through
summer employment. After her first year in geology, Heather
tackled the major companies and worked for Noranda in Northwestern Ontario. Her next summer was spent in another area of
Northwestern Ontario working for Shell. After third year,
Heather accepted a position with Shell in SE Nova Scotia near
Yarmouth. This summer she will be back in NW Ontario working
for AMAX
And then
who knows???
Thesis Topic: Paleomagnetic Study of the Quaternary
Sediments of the Goderich Basin, Lake Huron.
The natural remnant magnetism of the lake bottom sediments
of the Goderich Basin, was used as a correlation factor
between two cores retreived from there. The paleo-declination
and paleo-inclination values obtained from the sediments were
plotted versus depth. Correlateable peaks represent sediments
of a comparable age.
This method of correlation was found to
apply to sediments of a small basinal area as well as to the
Great Lakes area.
'

.

Randv Farmer
I'm one of the 'fortunate' few doing a structural thesis.
At least, everyone tells me I'm doing a structural thesis.
Basically, I'm looking at a small lense of sediments about
five miles north of Thunder Bay. The general purpose of the
study is to determine from structural and textural evidence,
the relationship of the sediments to the surrounding rocks
and their nature of deformation.
I've spent two summers in the bush; The first one in
1978 with Falconbridge Copper and the other in 1979 with
Selco Mining.
With Falconbridge I worked in the Savant Sturgeon Lake area. Basically, we just lazed around on the
beach, and participated in the weekly Ignace to Sturgeon Lake
(for which I clocked the fastest time of 38
time - trials
Once in awhile we got bored, and
minutes), and went fishing.
looked at some rocks. My second summer with Selco was spent
in northern Manitoba mapping in gneissic terrain for base

metals
My future interests after graduating are to work the
summer, then take the winter off and do some travelling.
Then, I think I'll be ready to try and find permanent
employment in geology.

�Tim Howson

Now that my four years at Lakehead are finished, I can
proceed with my real interests.
I am presently negotiating
for a job as a taste tester with a large rum
distillery in
the Barbados.
During the off season I plan to work as a test
driver for Yamaha Motorcycles Incorporated and as a
fishing
guide in Northern Ontario.
My future geological interests lie in finding
the famed
diamond deposit of Northern Canada, which must be at
the
bottom of Hudson Bay.
Secondly, I would like to stake and
develop a small placer gold operation and rum
distillery on
the Yukon River
However, after several summers of uranium work, I
am
proceeding into real geology (so I am told).
I have signed as
a base metal geologist with Falconbridge
Nickel. The job
involves mapping volcanics near Snow Lake Manitoba.
Past work experience:
Summer 1977 - Mapping as a Junior Assistant with O.G.S.
near Sault Ste. Marie
Summer 1978 - Mapping and prospecting with Eldorado
Nuclear Ltd., near Uranium City, Sask.
Summer 1979 - Mapping with O.G.S. in the Grenville
Province near Bancroft

Bruce Jago
Hi there, I'm one of the lucky few who is working on the
Coldwell Alkaline Complex for a thesis this year. By-the-way,
the word 'Complex' is not misleading, not at all.'!
Long ago
and far away, when Lake Superior tried to become an ocean, the
Coldwell Complex was born. A deep seated mantle rock began to
melt and caused the formation of three related alkali rich and
silica deficient magmas to rise and form a roughly circular
intrusive complex. Associated with each phase was brecciation
of pre-existing rocks, the formation of complex pegmatites &amp;
possibly large scale faulting.
Indeed, before erosion lasting
for a billion years removed the land surface, a volcanic
ediface was probably present. My thesis concerns the description of the main rock units and their intrusive relationships at the western contact.
Lots of fun you ask?, you bet!
My summer experience in geology includes working for
Noranda in 1977, and Shell in 1978 and 1979. Each season I
was beating it around the bush looking for copper and zinc in
volcanic terrains.
Saw lots of wildlife, had a good time,
but broke alot of hearts. You see I met the cutest little
moose and.... But seriously, the best camps have women in them.
All oink oink aside girls, it's more like home with panty
hose hanging on the jackpines.
My interests in geology lie in gold, silver, diamonds,
strange igneous rocks and making money on the stockmarket. My
interests outside of geology include making my own hooch,
economics, the great outdoors, sports, women and antiques.

�.

!

.

Myra Kennedy
As one of the few females in geology at Lakehead Myra
is just like one of the boys. (Not even strip joints or
,

advertisements that come in plain brown envelopes ever
produce the expected traditional blush.)
A very hard worker Myra can always be depended on to
come to our rescue with the right answers for labs that are
due immediately.
She enjoys cross-country skiing (as long
as the wineskin is within easy reach) and playing squash.
Various aspects concerning food are also of great interest to
her, and she can really bake up a storm for those Christmas
socials
Myra was employed by the government for two summers,
first on a local Experience '77 program associated with the
Regional Geologist's Office, looking at scenic features of
geological interest in the area. The second summer she
worked as a junior field assistant in an ODM field party near
Sioux Lookout. After that, more cushy jobs became available,
and she spent the summer after third year as a research
assistant for Dr. Borradaile. This summer, employment with
Dr. Borradaile is again a possibility as well as work on her
master's thesis.
Myra's honours thesis is a study of structure and
metamorphism across the Quetico belt from Shabaqua to Raith,
Ontario. The study is essentially a traverse ( about 30 km
in length) along highway 17 and the CNR and CPR railway lines
A sociological study accompanies the thesis on the effects of
repeated blasts from transport truck horns while one is
clinging to the sides of large road outcrops - echo, echo!!!
,

.

W. Michael Lucko

Mike is a busy and hard working guy. Not only is he
subjected to the normal rigors of Geology IV, but he is kept
on the go by his wife Edna, and sons Eric, Randy, and Adam
(arriving during years I, II, and III respectively of Mike's
years at L.U.) This year Mike and Edna seem to have broken
their record.
The three boys (otherwise known as the terrors
of Dacre Street) are of great help to their father in collecting rock samples.
(They think the "pigs" are really neat.)
Mike has worked for the past few summers on the notorious
"Black Gang" at Northern Wood Preservers in Thunder Bay, thus
managing to be with his family. Mike and family are now off
to Mayo, Yukon Territory, where he will work as a mine
geologist
Mike's thesis examines the pegmatites ("pigs"), of the
Ouetico Belt along Hwy. 527. His study involves petrographic
description and appraisal of the uranium potential of these
pegmatites

V

�.

)

Murray M c Gill
Murray is a member of the famous High Street can you pass
He can often be seen around the
the pinch test? society.
geology department sleeping, &amp;/or slumped in his chair during
(Or better still, telling Ron what a nice new
lectures.
His favourite pastimes are being late
shirt he is wearing.)
for geochem., geophysics or hysterical geology by at least 5
minutes, and pointing out to Parker Jack how ugly his thesis
rocks look.
Actually, his real interests in life include becoming an
insurance salesman and doing fabric and strain analysis on
unpeeled banana peels.
Away from L.U. Murray is interested in motorcycles and
photography. And yes, now and then he glances at a rock or
"Rocks ain't no good 'less they got silver or moly in
two.
If asked about the future, he replies that
'em" is his motto.
he eventually would like to investigate some gelatenous orbs
in Europe and become a qualified motorcycle mechanic.
Murray's thesis is a petrologic documentation of the
major rock units at the western margin of the Coldwell
Complex, near Marathon, Ontario. Hopefully, this thesis,
when compiled with works by A. A. and B.J., will help outline
the complex geology of the western contact region.
Work Experience:
Geophysics and junior mapper with Denison Mines (N .W T
Summer 1977.
Geophysics and Junior mapper with Shell Canada Resources,
(B.C.) Summer 1978.
Mine Development work and Senior mapper, with Kaiser
Resources (B.C.) Summer 1979
,

.

.

Bill Palmer
In the beginning, geology was an interest of mine which
spanned both my public school and high school years.
I started
collecting rocks, minerals, and fossils when I was four.
I
found geology to be challenging in university, especially
second and third year
My summer experience includes uranium exploration in the
Nipigon area, and gold exploration by geochemical rock and
soil sampling in the Timmins district.
Falconbridge Nickel
was my employer for both jobs. Hudson's Bay Oil and Gas
Company employed me in Northern Ontario and Newfoundland in
the summer of '79 as a junior involved in geophysical surveys,
soil sampling, line cutting and stream sampling.
Besides learning about various aspects of geology during
the last three summers, other valuable lessons were learned.
For instance, repeating the same type of survey can often lead
to boredom, but with enough patience and perseverance, one
can overcome this.
The results are satisfying to say the least
My interests outside of geology include fishing, sailing,
motorcycling and badminton. Future endeavours will include
being a geologist and raising a family.

�Jack Parker
Jack is one of the more charming and intelligent young
geologists of his class, and is often mistaken for Robert
Redford. He usually manages to squeeze in time to do schoolwork in his very rigorous partying schedule. He likes to
arrive fashionably late to most of his lectures; that's if he
arrives at all. However, you can often find him huddled over
his thesis rocks with Led Zeppelin blaring out of a tape deck,
or sprawled out at an L.U. dance beating his brains with drugs.
If you ever want to contact this aspiring young man, his
name and phone number can be found scrawled on the walls of
most of the men's washrooms at L.U.
Tomorrow I'll get my shit together.
His motto:
Jack has been employed by O.G.S., New Jersey Zinc
Exploration, and Urangesellschaf t for the last three summers,
and will spend his fourth with Esso in the N.W.T.
Jack's thesis topic is a detailed study of a metasedimentary unit at Finmark. The objective of his research
is to determine the environment of deposition of the sediments,
and to explain the structure of the area.

John Scollie
One of the quietest guys in fourth year, John is a native
of Thunder Bay, and still lives within a block of where he
was born. Although part Italian, he doesn't go in for disco
dancing, dressing up, or dingle balls. He does enjoy
photography-, watching movies, playing golf, and relaxing.
One
of his favourite sayings is, "It's too much work".
Most of his summers have been spent painting cars, and
if you ask him nicely, he may demonstrate to you his prowess
with masking tape and a razor blade. Last summer though,
John got a taste of the good life, as an employee of the
university under Dr. Mothersill. Word has it that he drank
alot of coffee, played with alot of mud, cruised the tropical
shores of Lake Huron for a month, and still got paid.
Aside from finding a gold mine (or even a Titanium mine)
John's goals for the future include, one day, becoming as
good a photographer as his idol Ansel Adams. A great thinker,
John's philosophical outlook can be summed up in a quote
from Roseanne Roseannadanna: "It just goes to show you Jane,
If it's not one thing, it's another."
it's always something.

V

�1

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Best

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Geology

students

of

L.U.

REGIONAL DIRECTOR
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�3rd Year Geology
Eric Albrechtsons

Robert Bennett

Helene Bourdages
Scott Bruce

Burns Cheadle

Warren Clendining

John Etches

Terry Foster

9 *.
Larry Kovac
Bill Love

Paul Gertzbem

Rick Kemp
John Pearson

wsr

Nicholas Spence

Eugene Kent
Blair Kite

Mark Stevens
Ron Tweed ie

?

�Eric Alfreds Albrechtsons
...but, most folks 'round here know me as Ralph.
Certified resident and president of Nugent St., and member
of Paleontology Club.
Activities include gourmet cooking,
speaking Latvian (great way to meet girls!), patronizing
studio 2019, and generally striving to preserve a calm mind.
Work experience - Summer 1979: Urangesellschaf t Canada
Ltd., diamond drilling - uranium ex., Baker Lake area, NWT
Summer 1978: Hudson's Bay Oil and Gas Co. Ltd., base metals
exploration, Newfoundland.

Robert Bennett

My past work experience includes one summer as a "monkey
operator" up 'dere in Nor-dern Quebec (base metals exploration)
and one summer chasing hot (warm) boulders in Northern
Saskatchewan. Of academic interest to me are structural and
economic geology, while philately, cooking, and attempts to
furnish my apartment have provided welcome distractions from
the rigours of life as an L.U. "rock doc".

Helene Bourdages

My interests in geology are in exploration and mapping.
Last summer I had the opportunity to work underground for
Denison Mines in Elliot Lake as a geologist's assistant, and
enjoyed it very much. Next summer I'll be in Kirkland Lake
with Newmont Exploration. My extra curricular interests
include partying and sports.

�Scott Bruce

Scott was the "Phantom" of the third year
class. (Field school must have been tough, eh
Scotty?)
His field experience includes two
summers of geological mapping in the Timmins
area (in the good ol Abitibi greenstone belt).
'

Burns Cheadle

My main interests are maximizing leisure time, and
taking two years to write up a half hour thesis on the
stratigraphy of the Rossport Formation, for Roy Shegelski.
In my many hours I occupy trying to avoid the microscopes, I
write music for guitar, cross-country ski and play "cat and
mouse" with my wife, Sherri.
I worked as the camp slave for O.G.S. in the summer of
'78 and as a chauffer and aide-de-camp for Roy Shegelski in
the 1979 field season.
This coming summer I'll be working
for Mattagami Exploration as grizzly bait in the Northwest
Yukon Territory.

Warren Clendining
Married to a fantastic lady, (who just so happens to be
doing this typing), Warren's last few summers of work have
involved assisting various professors in their research.
This has encompassed such things as collecting mud for Dr.
Mothersill, rowing Dr. Kehlenbeck around Hazelwood Lake, and
guiding Howard through the wilds of Fort Frances (and
surrounding bush). Geologically speaking, the things that
interest him most are geophysical methods (yawn)
and
structural geology. Beyond this lies a strong interest in
music - more precisely the trumpet - to which professor
Kehlenbeck can attest (not detest) to the devotion.
,

�John Etches
Two summers ago, with some reluctance, I began my life
as a geologist working for W.G. Wahl Ltd., in NW Ontario
It was she
(lugging rocks for a party chief named Betty)
that gave me my first insight into the geologist's world,
while teaching me the ways of the bush. I met greater
challenges last summer in the delineating and prospecting of
radiometric anomalies for Amax in NE Saskatchewan. This
.

years field season will be spent white water kayaking, big
game fishing and mapping for BP Minerals along the
Coppermine River, NWT.

Terry Foster
The summer before last, I chased women on the beach. This
past summer, I chased caribou on the tundra. This summer. I'll
be chasing women and anomalies around Wawa for the Algoma Ore
Division. My ambition is to catch all of the above.
(But does he know what he'll do with them if he catches
J
them?
.

Paul 'Jethro' Gertzbein

m
&lt;

jf

The last two summers I've been working in the Arctic,
looking for uranium. During the last two winters, I've been
1
partying to make up for what 1 missed during the summer,
hope to be going back up to the NWT this summer to do some
mapping for Gulf Minerals. I hope to make a career out of
exploration geology and getting high.

V

�.

.

Rick Kemp
Ambitions: - finish his honours degree
- an international job which requires his
presence only when he feels like it
Rick will surely be the proud father of about 3 young
geologists - 2 boys &amp; a girl. His confident manner, careful
and articulate speech, and easy laugh will get him a supervisory position with some tax evading corporate giant,
drinking 20 dollar scotch whiskey. Best wishes Rick.
Pet Peeve - Shopping with Larry.

Eugene Kent
Basically, I am a quiet unassuming individual. However,
In my case I realized, that
inspiration may come to any man!
if God or evolution had meant for me to 'live' in the lab,
then I would perforce have grown a universal stage, or
In the
perhaps a set of coloured pencils in lieu of fingers.
absence of these physical accoutrements, I have resolved to
become an exploration geologist - specializing in wine, women,
and song

Work experience - Summer 1977, Falconbridge Nickel,
Northern Ontario (Junior). Summer 1978, Derry Michener and
Summer 1979, Norcen Energy,
Booth, Wisconsin (Junior).
Uranium City, Sask. (Senior Mapper)

Blair Kite

Work Experience:
1978 Amoco Canada Ltd., as a monkey operator near
Matagami, Quebec.
1979 Falconbridge Copper, as a Galley slave at Savant
Lake and Schreiber, Ontario
At present:
Vice president in charge of mining with
Nugent St. Mining and Exploration
Special interests: Setting down by the fireplace with a rum
toddy and a goood ore petrology text on a long and dark
winter evening. Other interests include alcohol absorbance
and gourment cooking.

�.

Larry Kovac

Larry has aspirations of outdoing Alan Alda. All
kidding aside (chicken dinner) Larry has a beautiful
outlook on life - just ask Nick. For his life work, I
don't know: he has a rare insight in life: sees himself and
others as they really are. Larry may earn a living with
some multinational corporation, but, life has something more
rewarding in store for him.
Pet Peeve - Shopping with Rick.
I hope he makes more chocolate cake.
P.S.

Bill Love
I spent my first summer risking sterility looking for
uranium. My second summer was spent braving the jungles and
taverns of Northern Quebec in the pursuit of the most noble
of the metals - Gold.
This coming field season will be
spent working for the "feds" north of Yellowknife.
My principal interests are cross-sountry skiing, running
and mineral collecting.

John Pearson
(Alias - The Canadian Gigolo)
On the weekends I'm found competing with "Mr. Bill"
for the most time spent in "the lab" (that is not a disco
folks)
or just being myself and getting picked up in
(Are these potential
restaurants by cute? waitresses.
future Mrs. Yucks?) During the week I am kept busy with my
duties as Vice President of Exploration of Nugent St. Mining
and Exploration and many luncheon meetings of the
Paleontology Club. My past summers have both been in the
uranium field. Summer 1978: Conwest Exploration, Junior
Assistant, Northern Saskatchewan. Summer 1979: Senior
Mapper, Urangesellschaf t Baker Lake area, NWT
,

,

�Nicholas Spence

My interests lie in the smutty side of geology, such as
megalopoliths and the bucking and grinding of orogenic belts.
However, sometimes I have my serious moments and drift off to
I have had the good fortune of
the land of "Mega-Zircons".
It felt more like "Two Years
spending a summer in the bush.
Before The Mast". Flying, world affairs and suntanning on a
yacht off the Great Barrier Reef of Australia all the while
drinking Singapore Slings are amongst my other interests.

Mark Stevens

My first summer in geology was with Falconbridge Copper
Ltd., working in the Savant Lake area just north of Thunder
Bay, looking for base metals.
The second summer was with
Urangesellschaf t Canada Ltd., searching for uranium in the
Northwest Territories. For the coming field season, I will
be working for Petrocan in Calgary and the N.W.T.
My main interests are girls, water skiing, and
motocrossing

Ron Tweedie
I learn much while in attendance here; it's not always
related to geology however.
The biggest thought in my head is to find a mate.
Everything else will fall into place by itself. My ultimate
calling is not geology, but this degree will help me.
Dozens of taxi passengers have received various lectures
They all
al
re. evolution of the nor' westers range et
seem amazed, and exit the cab enlightened and grateful (big
It's a credit
tips) with smiles to face a different world.
to my lecturers one and all.
.

.

��2nd

L.

to R.

-

Year

Lupen (ed. note - maybe we can get him to switch to geology),
Ian Campbell, Brett Barnes, Eleanor Sidey, Tim Twomey, Cathy
Butella (another potential geology major??), Rob Dubyk, George
Chomacki, Keith Dailey. Absent: Mike Schulze.

Ian Campbell
Bret t Barnes

As a recruit fresh from the working class,
one of my main interests in geology is the
graduate employment rate. A geological summer
job exists somewhere out there, I just don't
know where as yet.

I began university in the Forestry degree
program, but switched to geology after 2 years
when I found summer job hunting to be a full
time job itself.
I spent last summer working
on Gulf Minerals Great Bear Lake project.
This
summer I'm headed to Northern Saskatchewan on
the employ of Eldorado Nuclear, and once
again on the search for uranium.

�)

.

George Chomacki
The summers of '78 and '79, I spent working
My geological interests are
diverse with an underlying motivation to
succeed academically.
Favourite activities include canoeing, flyfishing, hunting, and Nordic skiing.
(Was the
undisputed backgammon champ of the Dubawnt Lake
area
in the N.W.T.

.

Keith Dail ey
Interests in Geology - Basic, intend to
make it a living some day. Maybe add a new
dimension to oil exploration in Trinidad.
Summer Employment - Observing features of
interest on the beaches of Trinidad. Hope to
be more successful this year

Robert Dubyk
Thus far I have spent one summer working
in the office in Thunder Bay, and in the
Atikokan area for MNR - OGS
Outside interests;
I'm involved in carrying a portable office in
a brief-case and working in a darkroom.
.

�.

Mik e Schulze
I'm
I'm having a good time at L.U.
looking forward to summer field work and am
interested in mineralogy, as well as generous
amounts of partying and being outdoors away
from urban sprawls.

Eleanor Sidey

Due to the fact that no one will hire me,
have never been employed in any geology
related fields. I am in second year, but at the
rate I'm going, I hope to graduate within the
next decade.
I

Tim Twomey
Hi!
I'm in second year geology (mostly).
I've spent 2 summers in the bush. My first
summer I met Jack Parker who showed me the way
to geology and drinking.
Last summer, I broke
my leg midway through the field season and had
to spend half the summer at home, at the beach
in my cast and getting fully paid.
See you at the Prospector's Convention in
Toronto

�b.chcadlC.

�6

�PIEID TRIPS
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THE (9-4 IRON ORE BAR
IN TH? WORLD!

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                    <text>1984-85

�On the pnmordtal shores of Lake Tamblyn an assemblage of homin tds
gathered
0

0

0

Bahhhhhhhh

eannnnnnnn

eannnnnnnn

Bannnnnnnn
eanhhhhhhhhh
Boom Boo m
Boom Boom
Boom Boom

Boom Boom

Boom Boom

Boom Boom
Boom Boom

--

- ---

�.
/

and a certain bug who travelled by tram ..... .

. ..
(

�THE
PLATT - MITCHELL
OROGENY
...... created the environment and also introduced
a new predator to the populace.

R.T F:Q

" Belt up you lot"

HOME OF THE PREDATORS
Eutectic temperatures
in eutectic proportions

The
great wooley
hairy

razor-backed .............. Leitzosaurus .

...

�Dave "Guido" Glidden- cofounder of the " It is not enough
that I succeed, others must fail ," club.

Bruce 'ego'

THE NICHE· ·2019'

0!

�- Some survived the
orogeny by braun ............. .

"Boy Gord"

"Gordo" Sobering

..... some used brain

Shawn "Fingers" Aris

Adrian "Papa" S1monivik

..... and Still others

.... got by with a little help from thelf friends

�Robin James
Functuated Equil1br1um and
geography cla1med this species
He's now migrated to a colder Climate
and is adapting qu1te nicely with the
aid of snowmobiles.

Rick Wauhkonen
Punctuated eq.uilibrium
led him to math and
geography

~

Bojan J. Slfrer
A planktonic floater is now flourishmg
at McMaster
Geology (again)

~J.l.J~"r'1

�THE
BORRAIDALE- KHE LENBECK DEFORMATION
Graham Borradaille

wasn 't sure how to spell it
so I used both - ad
What else can be sa1d,
a picture is worth a
thousand words!

Manfred Khelenbeck

Geology's answer to Tom Selleck
Steve Kissin

Finally ........................... .
by this, the third event to
effect the populace, they
were beginning to learn
something about their
environment.

"Yes Lads, this is a rock!"

�In time members of the tribe began to establish the1r own niches
within the pecking order of the population.

Gary Forbes

Jennifer "Duff" Smith

.

.

????
..

Dave "Hide his books" Glidden.

�Let's take a look at these hommids m
their own env1ronment.

Adrian Shimonovik displays
mnovat1ve survival technique.

an

What ever gets you through ....... ........ .

Craig K. Alford

the pressures.

The Bell Boys

Living proof that
there is life after

lY..

Doug Parker

Sharon Bottomley

�,

Sharon
Bottomely

Dave "Delta Bravo" Bel

Pete " the meat" Gurney

Carol Lormand

��More candid shots of the hominids in their day to day ....... .

Geologist.. ..
.... Dr. Bartley
will be proud

Can anyone
forget
X-ray Tom!

"THE STUDY"
The "Brief Case Boys"

�Celebrat1on t1me among the anthropo1de1
Gene " V1d1ot' G1bbs
author of the famous shotgun answer

The Phantom Geolog1st

Doug Parker

��FIELD SCHOOL - HELL

ON WHEELS !-- - - - .

in search of the wicked rock beast the nomadic
hominids travelled far and wide - undaunted by
countless perils they pressed on in hopes of catching
the wild rock beast. The tribal elders had spoken many
times of these beasts telling tales of horror and evil.

Uh! What's a rock?
Members of the tribe
tracking the vicious
rock beast.

Lunch!!!!!

I think I've found
one!

They stalked it from the bushes.

In

many cases
they armed
themselves with
their primitive
tools and
performed tribal
dances.

�Rick Schuster

The trip was very rugged .

The elders told many stories about the
vicious rock beast.

�They pressed on through all maner of weather conditions searchmg everywhere for the
beast.

Relaxing along the way.

�(I know it's an joke, but I'm running out of material)

Geologist: A screnltst who w on't take Noah
for an answer

Finally ....... they found the creature

Lunch stop!

A Northern Ontario Musquito!

And so we say farewell to
our roving ban of hominids!

...... ..and killed it!

As the sun sinks slowly in the west

��-The fourth event to effect the "2019" basin- probably the most deadly of
them all- THE BARTLEY TECTONISM ....... .
th-is invovled major faults or more to the point fault finding and was
accompanied by the Jago Intrusion .
Kimberlites
in Northern Ontario.
The "Dawson Road Lots"
The yellow brick road
school of geology.

In search of the elusive northern
Ontario outcrop.

" I think I've worked it out!"
Those tall green things aren't outcrops!

�THE WESTERN INTER-UNIVERSITY
GEOLOGICAL CONVENTION
LAKEHEAD 1985

WIUGC Comm1ttee 1985 , c / o Depa rtment of Geology , Lakehead Univers1ty
Oliver Road , Th under Bay, O ntari o. P7B 5E1
Mark O'Brien

Injury sustained from "kicking ass" during conference

ff/Af{ K~
f: LOIJ

CHRR T

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...........1----.

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o.k . . .. whtt.r¢ do wa. ?
pu.£ i...ha.
t&lt;J1 .

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.----"--,1

~

jac ra

Chairman Flood

a
Reebtone's R '
lOti

\
embracing the coveted Dalmationite.

�Message
from
M. W. BARTLEY

�-Then there was the hours upon hours of calculations, drawings with numbers and
numbers and more numbers. Longer numbers than anyone had ever seen before or
wants to see again .
Yes- you remember THE PIT!

Here is a pictorial representation of the pit we designed in the "Major Problem" ...... it
looks like we do have a problem!

Patience is a virtue,
Possess it, if you can,
It ' s never in a woman ,
And seldom

found in man,
and

It at first you don't succeed,

Try, try, try again.

�GUESS WHAT!

IT'S THAT TIME OF YEAR AGAIN!

Guess what! It's final exam time again. Heh heh

�O.K. It's exam time, you're so upset, there's so much to do, your thesis, study
those case histories, and what about all these geophysics labs and equations? Well
that's it you are sure you're going to die.. Well here is a handy dandy guide to follow
that should help you determine if you're really going to die ..... .
If you're about to d1e, you'll begm to notice several terrifying sensations and
cosmic revelations as the phenomenal ve1l is ripped away, revealing, for the first
t1me smce the last time you passed away from the organic world, the endless,
eternal, unveiled kingdom of the vo1d
At the same t1e, you'll experience a mmd-numbmg personal cataclysm as you're
hurtled at twice the speed of light into a dark and unknown world in which
everything seems almost the same as 1t was before, only more so.
Don't worry about those strange new feelings and cosm1c thoughts. They're not
Important. After all, you're dead I What more can happen? After you've taken rebirth
you'll be able to look back on all this and laugh.
These sensations are useful for anticipating your exact moment of passage. And
1f you've had lots of previous practice, you will be able to use these sensat1ons to call
forth a senes of special psychological, emotional and instinctive mechanisms,
which will help you maintain a sense of eqUIIibnum--albeit false--during the total
loss of memory, vision, sensat1on and identity you'll experience as you are dragged
inevitably through the protal of death.
It's so easy to just expel your last breath 1n a s1gh of relief and fall facefirst into
your plate of spaghetti and meatballs, m total surrender to the perfect, shinmg,
endless vo1d, wh1ch 1s w1thout ObJects, states of consciousness, Identity, time,
space, filled parkmg lots and those empty weekends you've been struggling to hold
onto When you have finally g1ven up the effort of tryinc to maintain your organ1c
headbram personal1dent1ty, you'll understand the mystique of peanut butter by the
spoonful.
As the ve11 is lifted. you'll feel several sensations grouped together as a series of
symptoms, the first of wh1ch is a heavy pressure, like melting into an all-wool umon
suit while wearing a pa1r of lead boots Don't worry about this; you've probably got a
good 15 to 90 minutes left to handle any last mmute details, and if you have a friend
v1sitmg your death bed -- and your fnend IS so mclmed --you still have time for a
wonderfully refreshmg foot massage.
The second sensation will be a clammy coldness alternating with sweating, as if
your body were burning up. This 1s just one symptom of hypothermia, in which the
body's heat is reduced to lethal levels, Hey, nothmg to worry about- passage is still
mmutes away!

�The third sensation is a definite feeling that your body IS about to explode. You
may actually feel that you've been blown to smithereens and dispersed by the wind.
Now, you have somethmg to worry about! Passage is only moments away. Try to
relax and think of something pleasant.
The fourth sensation isn't really a sensation - it's a total lack of sensations.
Suddenly, although your mind has miraculously opened up and provided a
breathtaking and profound view of all creation, it doesn't refer to anything. This
vision plus 80 cents will get you a one way ride on a city bus.
In addition to these sensations, there may be other feelings, psychological
events, interludes, fugues, or other minor disorders, which ocur prior to passage
from the orgainc world to wherever you're going . You might experience a loss of
control over you facial muscles, causing an insipid smile or that unoccupied look
usually reserved for grad students.
You might periodically lose your hearing, or words and phrases that made sense
before might not make the same sense they made before when you understood
what they were saying by the words and phrases they might be understood and
made sense before when you understood what they meant by what they said to you
as you were listening .
There may be a loss of sight or radical changes in your vision vision v1sion. Your
breath might be ragged, particularly is you're getting more than just a foot massage.
It is possible that you will find yourself shivering or sweating and havmg an
uncontrollable desire to remove your clothes and walk around. Unless you're
expected to recover, this may well be a good idea. Who knows what last minute
adventures might be m store for you?
You may feel a lethargic calm descend over you . If you've spent your life on a
graduate fellowship or as a government employee, you probably won't notice th is.
There might be a loss of attention, caused by falling over unconscious on the floo r.
You may notice that your breathing stopped several minutes ago and that you can't
move your limbs. In this case don't bother trying to talk.
When all these symptoms of approaching death have been completed , someone
should gently whisper the following words into your ear: "So long sucker, you're on
your own."

�STUDENTS MESSAGE
'

'

. ,.-:: .
I~P~E. FOR THE UNGRATEFUL

WE THE WILLING, LED BY TttE Ul'jj(bl
ARE DOING. THE

' ,

'· \ •,

WE HAVE DONE SO MUCH FOR SO LONG, WITH SO
WE ARE NOW QUALIFIED TO DO ANYTHING WITH . .

�NOW IT'S TIME TO PLAY
MATCH UP THE QUOTESI

All you have to do here is match the quote with who or what said it.
Ready ..... .

QUOTE

PERSON

Unlike other people in this class I
treated this test as a closed book
one.

Terry 'Rex ' Sinclair

I'm so dedicated , it's fucking
u nbel ieveable.

Leslie 'Little Red' Mortimer

I'm calling you on that one you
boatanchor.

John DeVaney

Come to bed, Eugene.

Dr. Edward Mercy

You give an A student a screwdriver
and they'll stab themselves.

Dave 'Guide' Glidden

We're going to study the effect of the
environment on orgasms.

Dr. Graham Borradaile

It's so small I can 't find it.

Mark O'Brian

Why do they call it the sucker zone?

Dr. Phil Fralick

(Upon finding a unconscious John
Devaney laying in his own vomit)
O.K. who's going to take the first
kick?

Dr. Steve Kissin

In actual fact, all of this is neither
here, nor there.

Dr. Phil Fralick

To determine the sphericity of a
grain we must circumcize it.

Doug McKay

I don't know of any organisms with
triangular assholes.

Dr. Phil Fralick

Distribution in, uh, time, ah, and ah,
space.

Terry 'Tex' LaChapelle

�THE

STAFF

To the profs;
We may not have always agreed with you,
but once we realized we were right then it
was easy to allow you to have your opinions.
(Sorry, no pic for Maureen and Dianne. And
thanks Dianne from all the thesis students
for all the thin section work.)

A salute to the guys who really do the work,
the T.A. 's. We'd like to extend heartfelt thank
you's to those who dauntlessly marked our
junk and tried to read our scrawls.
Kevin, John, Dave, Dennis and Boris.

�Dr. uh, urn, Mothersill
ah, uh, urn, left us, ah
urn, for, ah, school, urn,
ah, in, oh, urn, Victoria,
urn, er, B. ah, C.

Dr. JOHN MOTHERSILL

The 'Hoot' has finally polished his last
section. They may shoot horses, or put
th e m out to pasture, but for
technicians, they just send them to
Scotland for a holiday.
(Now who's going to give students shit
for coats on the desks and keep our
profs in line.)

RON BENNETT

�The true test of a University is not the discoveries and inventions
which it's professors make or the books they write, but the sort of people
its students turn out to be ........ .

. ..

~~ .
~~

&gt; _/

-=--

�THE POETS (?) CORNER

STt,FF PHILOSO, 'HY
Rhodochrosits is red,
Azurite is blue.
The profs said to the students,
We'll FUCK YOU!

MY FAVORITE MINERAL
They call her an alkali amphible,
because of the end member position she stole.
To have a cleavage such as she,
is better than a distinctive 2V.
Sodium, calcium, magnesium, aluminum and silicon
She does contain,
her sisters are beautiful green and blue richterite
and glaucophane.
There can only be one similarity between the slug
and me,
it is mboziite, we love thee.

HEY! IT'S TIME AGAIN TO
PLAY MATCH THE QUOTES!
QUOTE

How many times did you
walk over the Hemlo deposit?

Mark O 'Brien

It's intuitively obvious
that I'm a short pervert.

Dr. Graham Borradaile

Obviously these striations
on this outcrop were
produced by someone on a
Ski-doo striving for Jerk-dom .

Sharon Bottomly

After all, I don't rea lly
care about the students.

Leslie Mortimer

It's O .K. Eugene I'm an
early riser.

Dr. Graham Borradaile

What ethnic groups make good
d rillers Dr. Bartley?

Dr. Roger Mitchel

Everyt hing we taught you in
first year was a lie anyway .

Dr. Robin Platt

.

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. .. .. . - . . ;·.i~-:.•:'!· • HARVEY, Pete:
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,-• LACHAPELLE, Terry: President of IGA. '·';',1.';',1
.
.
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Pres1dent, ch1ef and only ptlot of Harvey A1r Serv1ce
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:;-,!,•; operatmg a fleet of one piston bangers through Canada's •)'...',.., ~..•1..: :..•
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north serving prospectors, fishermen and breakfast
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-' •LORMAND Carol:
.
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on our early monng flights!
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'•· Sttllm search of the perfect soloflex man.
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·.!.";•!,•• MARTIN, AI:
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Develops theory that Australia IS on mass1ve K1berllte .• •• •.•.;
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The standard format of a yearbook is to incl
several messages from the faculty etc. I should
like to say at this time that had you not noticed it,
this is not a traditional yearbook. I have every
faith that each of us have memories of person or
persons who have greatly infulenced our lives. It
is in this spirit that I say at this time that this
yearbook is dedicated to all your memories.
It has been assembled in the pursuit of fun and
frivolity with no malice intent, however I am
aware that some may take offense, if that be the
case 1 suggest that you not read it.

Also, there is a distinct lack of material from
the other years due largely to the fact that they
didn't get off their butts and submit any material.

�\

1985 THE YEAR WE GRADUATE!

�COLUMBIA GRILL
&amp; TAVERN

SAUCE RIVER
LUMBER CO. INC.

I&amp;M ELECTRIC
REBUILDERS L TO.

GEORGE 0. HILL
SUPPLY LTD.

123 May Street South
Thunder Bay Ontano
623-7321

95 Cumberland Street North
Thunder Bay, Ontario
345-2982

580-B Squier Street
Thunder Bay, Ontario
345-3151

706-724 Balmoral Street
Thunder Bay, Ontario
623-4447

A.R. MacLEAY L TO.

HOWARD M.
GRAHAM LTD.

ALMEIDA
UPHOLSTERY

BEARING SUPPLY
(CANADA L TO.)

920 Memorial Avenue
Thunder Bay, Ontario
345-2352

1112 Russell Street Unit 1
Thunder Bay, Ontario
623-2131

General Insurance Adjusters
115 May Street South
Thunder Bay, Ontario
623-3468

ACADEMY
HAIR STOP
558 Beverly Street
Thunder Bay, Ontario
344-1551

HOSTESS FOODS
125 Gore Street West
Thunder Bay, Ontario
577-2551

Ontario Land Surveyors
280 Pearl Street
Thunder Bay, Ontario
344-7561

BLUE PARROT
376 Usgar Street
Thunder Bay, Ontario
345-5345

UNITED GRAIN
GROWERS L TO.
106 Cumberland
Street North
Thunder Bay, Ontario
344-0778

Fruit &amp; Vegetable Patch

HOLLYWOOD
HAIRSTYLING

386 Cumberland
Street North
Thunder Bay, Ontario
345-8090

1101 Arthur Street West
Victoria Mall
Thunder Bay, Ontario
577-5621

J&amp;M MINI MART

THE LOVE BUG
714 May Street North
Thunder Bay, Ontario
622-1030

BUSINESS SUPPLY
COMPANY

HORNETS SPORTS
ENTERPRISES L TO

113 May Street South
Thunder Bay, Ontario
623-8476

THE UNIFORM
SHOPPE

300 Simpson Street
Thunder Bay, Ontario
623-4462

1000 Fort William Road
Thunder Bay, Ontario
623-5442

ALMOST LIVE TAPED
SOUND
ENTERTAINMENT

NATIONAL PRIDE
CAR WASH

PPG CANADA INC.

598 Arthur Street West
Thunder Bay, Ontario
577-3331

1056 Memorial Avenue
Thunder Bay, Ontario
623-9505

106 North Windermere
Thunder Bay, Ontario
345-2874
After Hours: 345-8771

THUNDER BAY
INSULATION &amp;
SUPPLY LTD.
R.R 17 Oliver Road
Thunder Bay, Ontano
344-5667

THE LAKEHEAD
ANSWERING
SERVICE
223 M cKellar Street
Thunder Bay, Ontario
622-7748

CUMBERLAND
BOOK STORE

THE FRAMING
EXPERIENCE

20 Cumberland Street North
Thunder Bay, Ontario
344-4202

1186 Memor ial Avenue
Thunder Bay, Ontario
623- 1661

TRAILER WORLD'
A.A. 17, Oliver Road
Thunder Bay, Ontario
344-3332

THUNDER BAY
COMMUNITY
CREDIT UNION INC.
29 Court Street N.
344-6639

CENTRAL CANADA
EQUIPMENT
(Thunder Bay) LTO.
1055 Commerce Street
Thunder Bay, Ontario
475-4255

TRAILER WORLD
A.A. 17 1114 Oliver Road
Thunder Bay, Ontario
3«-3332

DeL Can
DELEUW CATHER
CANADA LTD.
1204 Roland Street
Thunder Bay, Ontario
623- 1772

MEMORY DIAMONDS
317 Victoria Avenue East
Thunder Bay, Ontario
623-8943

ITS A
GOOD TIME
FOR THE

GREAT TASTE~

rA1

�Our thanks to the following patrons who contributed to the success of our yearbook by means of listing with us.

LAKEHEAD UNIV BOOKSTORE
Oliver Rd ., Lakehead University
345-2121
MATFRA MOTORS
528 Syndicate Ave. S
622-4021
THUNDERBAY COSMETOLOGY &amp;
ELECTROLOGY CLINIC
2nd fir., 40 N. Algoma
345-5632
RED RIVER TEXACO
914 Red River Rd.
767-7811
R.P.M. DRIVES &amp; DESIGN INC.
1165 Russell St.
623-6481
NU-LUSTRE CARPET CLEANERS
170 Maxwell Ave.
767-8101
LAKEHEAD ROOFING
R.R.1, 1450 Rosslyn Rd.
577-6476
R. CORAZZA L TO
687 Harold Cres
623-3445
CHARNOCK JEWETT BURMASTER
CHARTERED ACCOUNTANTS
400-101 Syndicate Ave. N .
622-9608
SUPREME CLEANERS
425 S. Syndicate Ave.
622-6411
ED'S TEXACO SERVICE
273 Shuniah St.
344-6181
FRANK'S LAUNDROMAT
227 Algoma St. S.
344-3801
MARG'S PRINT SHOP
1135 Russell St.
623-4646
GRAHAM, BACON, WEL TEA ARCHITECTS
179 Algoma St S.
344-5721
HOITO RESTAURANT
314 Bay St
345-6323
GIANT TIRE SALES
330 Fort Wilham Ad
344- 1531
THE MATCH BOX IN THE MALL
Lakehead University
344-3791
TROPICAL FISH AND PET SUPPLIES
285 Grenville Ave.
683-8859
INTERCITY WELDING &amp; FABRICATING
(Thunder Bay) Inc.
552 Twelfth Ave.
345-1877
CA JOHNSON ELECTRIC LTO
544 Wmnipeg Ave.
345-0531
FORGET-ME- NOT GIFT SHOP
109 MaySt N
622-9474
E K T INDUSTRIES INC
1100 Russell St.
623-5211
COLQUHOUN'S IDA PHARMACY
502 Victoria Ave.
623-7464

FORT WILLIAMS GARDENS
901 M1les St
625-2929

DR K A JACOBSON DENTIST
101-59 Court St. N
344-7982

PLATA &amp; MORRILL
CHARTERED ACCOUNTANTS
596 Squ1er Street
344-6684

ST DOMINIC'S CHURCH
130 Redwood Ave.
577-5672

E L A SMITH BROKERS L TO
119 S MaySt
622-6831
C. D HOWE CENTRAl.
95 Cumberland St. N .
344-7218
THUNDER BAY TRUCK CENTRE
1145 Commerce St
577-5793
JOHN'S SAW SALES L TO
243 Manitou St.
345-5551
"COMPLIMENTS OF A FRIEND "
PARADISE MOTEL
221 Arthur St. W
577-8686
BEACON HILL LODGE
135 Vickers St S
623-9511
AFNOO
204-14 Rue St. Paul
345-5092
EMILIO BARBER SHOP &amp;
HAIRSTYLING
130 Brodie St. S
623-6342
INTERNATIONAL GIFT SHOP
2Q-230 Park St. Keskus
344-8232
IMPORTED ORIENTAL FOODS
270 Cumberland St. N.
344-5118
ST ANTHONY'S PARISH
36 Banning
345-6482
HUDSON'S BAY VENDING
1160 Commerce St
475-4461
CASTAGNE'S ROCKS &amp; MINERALS
PO Box 2594, P7B 5G 1
983-2047
D S. McCULLOUGH REALTY LTO.
225 PhillipS
767-3329
SCIENTIFIC HAIR CARE
1020 Dawson Rd , County Fa1r Plaza
767-2871
MOUNSTEPHEN TAXIDERMY
244 E Christina St.
622-1879
DEL RONDO &amp; THOM'S TROPHIES
317 Victona Ave.
623-6942
COMPLIMENTS OF
DR JAMES H . T DONALDSON
1535 VIctoria Ave E
622-6455
A TO Z RENTALS
946 Cobalt Cres
622-4333
SEAWAY REFRIGERATION
121 Crown St
345-8333

AIRPORT RESTAURANT
Thunder Bay Airport
475-3364
THUNDER BAY FLYING CLUB
Thunder Bay Airport
577-1118
ST PAUL'S UNITED CHURCH
349 Waverly St.
345-5864
N . M PATERSON &amp; SONS LTD.
PO Box 644, P7C 4W6
577-8421
AMERICA TRAVEL
217 S1mpson St
623-2721
DEVON, KING. ELGIE OPTOMETRISTS
230 Park Ave., Keskus- 767-1355
County Fair Plaza - 345-8112
ERCO, A DIVISION OF TENNECO
CANADA INC.
1535 City Ad
623-7632
IRON RANGE BUS LINES INC.
294 Memorial Ave.
345-7387
V.B. COOK CO. LIMITED
CONSULTING ENGINEERS
PO Box 936, P7C 4X8
623-0461
OUR LADY OF LORETTO CHURCH
290 Grenville Ave.
683-8753
CARTER, GORDON &amp; JOHNSON
PO Box 2958, P7B 5G5
345-3361
FAVOT CONTRACTING LTO.
821 Vickers St
622-6591
VANDERWEES POULTRY FARMS
R R 1 Townhne Ad
935-2507
ONTARIO MOTOR LEAGUE
585 Memorial Ave
345-1261
BURGER KING
95 Ravenwood Ave.
623-4612
PITTSBURGH PAINTS
665-669 Beaverhall PI
577-4271
TALKING TOPS
Victoriav1lle Centre
623-7590
LAKEHEAD WINDOW CLEANING
810 N Brodie
622-9171
A &amp; I SUPPLY LTD
933 Tungsten St
623-5464
THE WIREMAN
S1te 15-39, R R 13, Thunder Bay
983-2298

�Our thanks to the followmg who contnbuted to the success of our yearbook by means of listing with us.
WORK WEARHOUSE
1092 Memo rial Ave.
623-2634

NORTHWESTERN BODY &amp;
FENDER REPAIRS
549 Tenth Avenue
344-8961

FORT GARY INDUSTRIES
91 5 Walsh St W
577-5724
J.F. THOMSON TIMBER L TO.
4A South Court
344-2132
ST. JOSEPH'S HERITAGE
63 Carrie Street
767-6225

PARAMOUNT PLASTERING
2726 Silles Court
·
623- 1395
MAY &amp; CUMMING SHELL SERVICE
231 May Street North
623-9302

DE LUXE SIGNS L TO.
170 Front Street
345-8111

AMERIGO CONSTRUCTION
1228 John Street
767-2557

BRENT PARK STORE
86 Brent Street
345-6931
TOWLAND HEWITSON CONSTRUCTION
Oliver Road
345- 1201

NOR SHOR READY MIX
610 Hewitson Street
622-6154
MOUNTAIN VIEW VARIETY &amp;
FIREWOOD SALES
A.A. 4, Box 162 City Road
623-1377

LENSTEEL LTO.
174 Powley Street
344- 1605

TWIN CITY LUMBER
1174 Roland Street
623-3953
THE SHOWCASE
Northwood Park Plaza
577-4442

MARIO'S BOWL
710 Memorial Avenue
344-9644

CLARA INDUSTRIAL SERVICES LTO.
1130 Commerce Street
577- 7546

CHAMPION OFFICE SUPPLY
SERVICES L TO.
115 North May Street
622-8111

PAINTED TURTLE ART SHOP
1-204 Red Rtver Road
344- 4636

KELLOUGH BROS. DAIRY L TO.
1703 Victoria Avenue East
623-6413

NEW CHINA TAVERN
470 High Street South
344-5861

FORD GLASS CENTRE
129 Vickers Street South
622-7701

INDUSTRIAL HARDWOOD PRODUCTS
LTD.
106 Street
622-8687

W.L.WARDROP &amp; ASSOCIATES
595 Squier Street
344-0865

A.M LUDWIG SAW SHOP
324 106th Street
622-7112

UNGMAN LAPRADE TRAVEL
SHOP LTD.
1020 Dawson Road, Country Fair Plaza
345-7222

CHAN'S RESTAURANT
130 May Street North
622-2601

OVERHEAD DOOR COMPANY OF
THUNDER BAY LTO.
615 Norah Cres.
623-6494

PETERSON ELECTRIC
142 Cumberland Street North
344-2471

FLIP-A-TOP
324 North Cumberland Street
344- 1732

D.D.&amp;B. CONSTRUCTION
204 Selkirk Avenue North
623-()002

THUNDER BAY ESSO DEALERS &amp;
MOORE FUELS
PO Box 632 Thunder Bay
P7C 4W6
623-3791
LAKEHEAD LUNCH
433 Syndicate Avenue South
622-9700
BREUKELMAN'S POTATO FARM
A.A. 6 Thunder Bay
P7C 5N5
939-2040

577-8471
307 Euclid Ave

767-6201
863 Red Rtver Ad

NEW FROM SUPERIOR

344-0711

T ' e11ft with CUl lOm fit

ediuatlbht terew arm~ for 220
., p end 300 h p crew* traciOt'l

231 Cumberland St N

623-2245

out front lor rnochlnebolance Good..,_ lor
m1nlmum aotl d'*turbence

.... ._

201 Syndtute Ave S

- c . . a . . _ u p lo 25

Young Driver•
of Canada

• W for camp u.. Euity moved
tn 5 mlnutee

----

Cuatom 8u1" Unitt
l.owong Tratlorl ancl T,..no
low Boy &amp; Po~ Trot""'

32 Algoma St. South,

F~I-&amp;IWOtypoo~

(807) 344-3821

Cab 51&gt;- &amp; ~ Tr..-

---

IJIN-Mor-

TRIFON"S
PIZZA

~

1180 I'IUSSELL ST.

~

..HONE 112.&amp;·•181

PROJECT MANAGERS
AND GENERAL CONTRACTORS
INDUSTRIAL AND COMMERCIAL

D11alare lor Jonearad

D&amp;R

Chain

132 Fairbanks Cres.

Equipment Rental &amp; Sales Ltd.
Bulldozing
Excavating

I000 8 I
w. -

Sa-

.. _,e.lng -Mil

SUPOHOII TJIAIURS

I

I

1185 Roland St Thunder Bay. O nl P7B 5G3

767-7647

Tal (107) 823-5107

Telex 073-4151

683-6261

Port Arthur Shipbuilding
P.O. Box 2690

�- - -.... GENERAL MA CHINE SHOP
FABRICA TIO N
WELDING

GRAHAM &amp; WHYBOURNE ZIEBART
725 N MaySt. Thunder Bay Ontario
Your To tal Appearance and
Protectton Centre

623-9121

FAIRBARN'S
Machme Shop ( 1983) Ltd

Gulf Agent

Messenger &amp; SmatJ Parcel Dehverv
Rad•o D•spatched
A ~rport Servtce

_

622-5111
623-5611
1116 V1ctoria Avenue E.

home in Thunder Bay
It's all here!

Beatrice

a

FRANK'S

O

Computer Systems Engtneerong
Law Ftrm Management Systems
General Accounttng Applications
Payroll
Word Processtng

(807) 623-2310

SERVICE STATIOII LIMITED
MALGOMAITI

345-5813

SPECIALIZING
• TUNE -UPS
• BRAKE SEAl/ICE
• EXHAUST SYSTEMS

IN
• FIRESTONE TIRES
• DELCO BATTERIES
• WHEEL BALANCING

!1 71 SYNDI C A TE AVE , 5 .
P 0 B O X .4 1!1
TH U ND ER B A Y . ONTARIO
P 7C .4VII

WILLIAM S. TOMLINSON . JR.
9 - BA N . CUMBERLAN D ST.

HENDERSON GLASS

T HUNDER BAY "P", ONTARIO

P7A

For

IBM, OLIVETTI
TOSHIBA. CANON
106 Somp10n Sll. .l

622-5338

llwn&lt;ler a.r. On111io P7C 3Ht

t'" ~_, ~ ~··1

r N w_ p_~__,

WDDD
PRESERVERS IN[.

P 0 Box 2990
Thunder Bay. Onlano P7B SG5
Bus (807)344·8451 Telex 073-4570

ODH

P HONE

3 45-9562

QUALITY DOOR
HARDWARE LIMITED
565 ELEVEN TH A VE .
THUND ER B AY ,

P7B 2R5

RIDGEWAY CLINIC
1001 Ridgeway St.
622-0601

I LA K ~H~AO ) LI M IT ~O

4L I

Ill

CO RPO RATION FALCONBRIDGE
COPPER

r=1

LAKEHEAD INTERNATIONAL
TRUCKS LTD.

r

~., 2606 Victoria Avenue East
Th under Bay , On~r~

P7C 1 E7

101 5 Daw so n Road
Thunder Bay, On tari o

Authorized Dealer

NDRTHE~N
Beatrice Foods (Ontario) limited
Klomp Wakeheld Dauy DIVISIOn
134 South Waterloo Street
Thunder Bay Ontar10 P7E 2C3
807 623 8233

G.K. Fleming &amp; Associates Limited

1118 Ro land St .

P7C 4Wtl

For a brighter furture. make your

CENT RAL TA XI
24 Hour Courteous Servic~

''

OPERATION S MANAGE R
L A KE H E AD S HIPP I N G CO. L TD

The Corporat1on
Of The Ctty 01
Thunder 8.1y

Tel. 807-623-3996

•
-

C HARLE S E . U MPHERSON

BUS 62~022

e

720 Hew1tson St

3 4!1 ·1 494

P 0 B OX 110 2
TH UNDER B A Y F O NT

623-1933

GINO ANTONIAZZI LTO.

Bus

767-1611

HOUSE OF MIRABELLI
MEN S HAIRSTYLING
Perms • Co lou ring
Expert B a rbering
lnterc1ty

Keskus

Countyfatr V1ctonavllle

345-5428

767-1647 623-3882

550 SqUier Street

PHILLIPS, WILSON
AND MILTON L TO.
AR lO LAND SURVEYORS
345-0574

3 10 N . MAY STREET
THU NDER B A Y. ONT.
P7C 3 P 9
TELEPHONE 623 · 33 22

Telephone 807/6 23 - 15 11

T ypewrIter
Out
Rentals Ask A bout

1

PrOMPT
PROFeSSIONaL

SeRVICE

POTTER PUMPING
SERVICES UMITED
IHOUSEHOlO SEPTIC &amp; INDUSTRIAL WASTE)

623-5811

SHERLOCK
8\ISINIM 8\'SI'DG LtD.

JACK TURNER BUS LINES

'"

1220 Com merce St.
T hunder Bay, Ontario

2400 ROSSI..YN RD. RA 1
TKJNOEA BAY. ONTARIO P7C 4l'J

COX FOOD
BROKERS
14 1 H ARD ISTY STR EET
PO BOX 273
TEL (807) 623-3366
TELEX 0734638

577-7486

Te l: 3.1,5-6581

LAKEHEAD MOTORS LTD.
951 Memorial Ave.

�623-0438

POULIN

OGILVIE MILLS L TO.
675 New Vickers St
PO Box 37

(_A_)

GHAT

wc s r

8:
lf.f

%/J,fb'L

q:::-

Ll M IT [ 0

LCJtVS {fftl

!4.

f£1 1B

J~ C antonese Sty le Brunch (Dem-Sum)

PHONE 344-8464

fro m 10 pm to 1 am Mo n. to Sat

595 Arthur St. Htghway 17 t moletromlheaorpon
Tel. (807) 577-5761

TELEX 073-4575
P. O. BOX 3170 THUNDER BAY, ONTARIO

P7B 5G6

VAN HORNE &amp; FRONT STS
PO. BOX2686.
THUNDER BAY. ONT P7B 5G2
TELEPHONE (807) 345-1435

NORTHWESTERN STEEL
(THUNDER BAY) LIMITED

RADIO SHACK

Rick Middaugh
lan Spence
L----.:...___
R fl • 14, AUCE AVE ,

~

Inter City Plaza Thunder Bay

....,

345-2042

aAY, OHT

..,..,.....,,

.,....)

ALLIIID C:OMPUTII.
C:I!NT.II8 INC:.
Sales, Servtee, Rentals
Computer Related Supplies

treatvou
royally

Authoruro Oealer

HAPPY TIME TOURS
Charters &amp; Pre-Planned Tours
Tel. (807) 345-0751P

......,,~,.,....

Systems Business Forms Limited
Bsmt. 2606 V1ctona Ave E.

623-2749

1..-.

.

122 W . FRI:OI:RICA ST.
THUNDER BAY ONTARIO

,., ,.., ,.....,;.,.,
623-J9JS

473-4755
201 5 SYNDICATE AVENUE

204 M ay 51 S
Karate Ktckboxtng
Weapons
Tap Ja.u Ballet
Aerobtcs Jazzerc '\tt

[!]

623-5694

Jri- J&gt;er/ecfion.

-

-

AMUSEMENT EQUIPMENT
SALES

-

SERVICE

~&amp; W Games

Ltd.

31~ Euchd A\enu•
Thunder Bay Ontarto P7£

'iG~

577-4200
577-4209

•

TOM JONES
CONSTRUCTION INC

GENERAL CONTRACTORS

560 Squ1er Street
345-0511

.L...t.;~ .1 !».,.,, J!..
RENTALS

395 Fort W1lltam Road

J.B.£.\'ftns

_ , ,..., 11:...... . lo.•

BILLIARD SUPPLIES

•

lli!JUI

jJf)J/

RU, AUTOMOBILf
&amp; UfE INSURANCE
IIIIIIIM·IJOIIE·~II
lEAL ESTATI
_

_ _ _ Lumtt:d_

OLAVI JARVELA
..[ GISTUED INSUIIIANCE IIIIOKEIII

634 SIMPSON STREET
THUNDER BAY. ONTARIO

TEL

(807) 622·5543

LAKEHEAD LABOUR CENTRE
Am. 9, 929 Fort William Rd.

SALES-SERVICE-PARTS
ACCESSORIES

BUS 345 7309
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107 623 7232

tElU 073 "360

344-9031

:..

We~!.~

121 East Avenue. P7B 5N1

(807) 345-8031

"

Furam Co urt

~X

RES 767·2149

210· l• N CUMIULANO ~TRU T
l l U THUNO(III lAY ON TAIUO , .

)G6

Cjl~
food service
DMSo&lt;&gt;n of Wesrtao1 Foodlll&lt;l
650 Ho1&lt;&gt;10 C&lt;oocen1
ThunOef Bay Onta1 10
P7C &lt;X6

622-6403

�JI~E~~TEl
ELECTRONICS INC.

GENERAL INSTRUMENT
SATELLITE TV SYSTEM

PASSENGER VAN RENTALS

COIIIII!RCIAL a COII.UIII!R I!LI!CTRONIC.
DI.TRIBUTION • •At•• •••RVICI! • RI!NTAL.
•TT7 ~- • TIUURIAY 0HW10

~ ·1'18

3Z7• 111071 ~

KLOMP WAKEFIELD DAIRIES
134 Waterloo St. S.

622-2169

~

Reserve Today!
557-5766

•

1475 W. Walsh St.

~

941 s;mP'on St.

~4$4).5

Major General
Contracto,.. In
Northwestern Ontario

622-9639

AVIS

FALINO'S SUPERETTE and BOOKMAG
198 S. A lgoma St.
Thunder Bay, P7B 389

Phone 345-9841
or 344-7687

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