The glacial geomorphology of the northern Nain-Okak section of Labrador.

The role of Labrador-Ungava as one of the main gathering grounds of the Pleistocene ice caps, and one of the final centres of wastage was recognised as long ago as 1896 by the government geologist A. P. Low. In spite of its obvious importance in the glacial history of North America, Labrador-Ungava...

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Bibliographic Details
Main Author: Andrews, John. T.
Other Authors: Parry, J. (Supervisor)
Format: Thesis
Language:English
Published: McGill University 1961
Subjects:
Online Access:http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=112967
Description
Summary:The role of Labrador-Ungava as one of the main gathering grounds of the Pleistocene ice caps, and one of the final centres of wastage was recognised as long ago as 1896 by the government geologist A. P. Low. In spite of its obvious importance in the glacial history of North America, Labrador-Ungava has received but scant attention from research workers in the field of glacial geomorphology or geology, due mainly to the inaccessibility and uncertain weather of the peninsula.