Late Quaternary geology and geomorphology of the Elk Valley, southeastern British Columbia

Glacial stratigraphy and geomorphology of the bottom areas of the Elk Valley support the existence of one major ice advance, presumably during the late Wisconsinan. Its retreat probably occurred in two stages by orderly frontal withdrawal. Glacial Lake Elk, formed within the Elk Valley from meltwate...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: George, H., Gorman, W. A., VanDine, D. F.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1987
Subjects:
Online Access:http://dx.doi.org/10.1139/e87-072
http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-072