Abstract
The author describes the survey of glacier snouts in the Duart Lake area. This is part of Canada's contribution to a world-wide study of the variations in existing glaciers, which was recommended by the Snow and Ice Commjssion of the International Association of Scientific Hydrology. He also considers the geomorphological and botanical evidence of the former extent of glacierization and compares the more recent phases of this process with those of other countries.

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