The Nastapoka drift belt, eastern Hudson Bay: implications of a stillstand of the Quebec–Labrador ice margin in the Tyrrell Sea at 8 ka BP

During deglaciation of eastern Hudson Bay, the western margin of the Québec–Labrador sector of the Laurentide Ice Sheet came to a stillstand about 8 14 C ka BP along the Nastapoka Hills, a series of topographic highs along the bay. These hills are the northward continuation of the eastern Hudson Bay...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Lajeunesse, Patrick, Allard, Michel
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2003
Subjects:
Online Access:http://dx.doi.org/10.1139/e02-085
http://www.nrcresearchpress.com/doi/pdf/10.1139/e02-085