Ice-Disintegration Features in Western Canada

The wasting Wisconsin glacier left predominantly till deposits in western Canada and only subordinate amounts of stratified drift. In the final phases of wasting, the ice separated in places into a large number of small, dead, ice blocks: it disintegrated. This disintegration caused the preservation...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	The Journal of geology 1959-01, Vol.67 (1), p.48-64
Hauptverfasser:	Gravenor, C. P., Kupsch, W. O.
Format:	Artikel
Sprache:	eng
Schlagworte:	Crevasses Flint Geology Glacial drift Glacial landforms Glaciers Ground moraines Ice Moraines Ridges
Online-Zugang:	Volltext
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