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...

Full description

Bibliographic Details
Published in:Géographie physique et Quaternaire
Main Authors: Duk-Rodkin, Alejandra, Hughes, Owen L.
Format: Text
Language:English
Published: Les Presses de l'Université de Montréal 1991
Subjects:
Online Access:http://id.erudit.org/iderudit/032847ar
https://doi.org/10.7202/032847ar