Age Relationships of Laurentide and Montane Glaciations, Mackenzie Mountains, Northwest Territories
The Mackenzie Mountains were glaciated repeatedly by large valley glaciers that emanated from the Backbone Ranges, and by much smaller valley glaciers that emanated from peaks in the Canyon Ranges. During the Late Wisconsinan the Laurentide Ice Sheet reached its all-time maximum position. The ice sh...
Published in: | Géographie physique et Quaternaire |
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Main Authors: | , |
Format: | Text |
Language: | English |
Published: |
Les Presses de l'Université de Montréal
1991
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Subjects: | |
Online Access: | http://id.erudit.org/iderudit/032847ar https://doi.org/10.7202/032847ar |