Lakehead University Geology - Journal Yearbook (Thunder Bay, Ontario Canada)

 - Class of 1980

Page 15 of 72

 

Lakehead University Geology - Journal Yearbook (Thunder Bay, Ontario Canada) online yearbook collection, 1980 Edition, Page 15 of 72
Page 15 of 72



Lakehead University Geology - Journal Yearbook (Thunder Bay, Ontario Canada) online yearbook collection, 1980 Edition, Page 14
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Lakehead University Geology - Journal Yearbook (Thunder Bay, Ontario Canada) online yearbook collection, 1980 Edition, Page 16
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Page 14 text:

CONGRATULATIONS AND BEST WISHES to the Graduates M. W. BARTLEY ASSOCIATES LTD. Geologists 209 Winnipeg Avenue Thunder Bay, Ontario the Lakehead University Geology Club Wishes all Students a very Successful Summer Exploration Season Rob Bennett , President John Pearson , Vice - President Join the Rest of the Crowd at the Crest y Crest Motor Hotel Red River Road and Junot



Page 16 text:

Dr. John Sydney Mothersill , B.Sc. (Physics, Mathematics) B.Sc. (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 east- ern part of Lake Superior and for the deep-water lakes in general.

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