The Nastapoka drift belt, eastern Hudson Bay: implications of a stillstand of the QuebecLabrador ice margin in the Tyrrell Sea at 8 ka BP
During deglaciation of eastern Hudson Bay, the western margin of the QuébecLabrador 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...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
2003
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Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e02-085 http://www.nrcresearchpress.com/doi/pdf/10.1139/e02-085 |