Late Quaternary Land Emergence in Northern Ungava, Quebec

Twenty-one C14 dates of material from Late Quaternary marine terraces are used to construct an isostatic uplift curve. The phase of rapid uplift averaged about 26 ft. per 100 years, while for the past 5,200 years uplift was just under 1 ft. per 100 years. Updoming resulted in an upward (southerly) t...

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Bibliographic Details
Published in:ARCTIC
Main Author: Matthews, Barry
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1967
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66344