About This Item

Share This Item

The AAPG/Datapages Combined Publications Database

CSPG Bulletin

Abstract


Bulletin of Canadian Petroleum Geology
Vol. 13 (1965), No. 2. (June), Pages 354-354

Abstracts of Papers: Jointing of Boulders Caused by Flowing Ice

W. O. Kupsch

At four different localities in southwestern Saskatchewan it can be shown that boulders, now part of an unconsolidated deposit, are fractured, presumably when yielding to stresses exerted by a flowing glacier. The stratified drift, of which the boulders are a part, is believed to have been cemented by interstitial ice when deformation took place.

A study of the mechanical behavior of materials under low temperatures, small stresses operative during a long interval of time, and other conditions assumed to have existed during Pleistocene glaciation, is called for.

End_of_Record - Last_Page 354-------

ACKNOWLEDGMENTS AND ASSOCIATED FOOTNOTES

University of Saskatchewan, Saskatoon

Copyright © 2004 by The Society of Canadian Petroleum Geologists. All Rights Reserved.

Pay-Per-View Purchase Options

The article is available through a document delivery service. Explain these Purchase Options.

Watermarked PDF Document: $14
Open PDF Document: $24