Pleistocene Montane Glaciations in the Mackenzie Mountains, Northwest Territories
During the Pleistocene the Mackenzie Mountains were affected by a series of glaciations. Through all the glaciations a single pattern seems to have been repeated: a Cordilleran ice sheet formed to the west of the continental divide and montane valley glaciers formed to the east. The montane glaciers...
Published in: | Géographie physique et Quaternaire |
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Main Authors: | , |
Format: | Text |
Language: | English |
Published: |
Les Presses de l'Université de Montréal
1992
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Subjects: | |
Online Access: | http://id.erudit.org/iderudit/032889ar https://doi.org/10.7202/032889ar |