The Quaternary History of Cumberland Sound, Southeastern Baffin Island: The Marine Evidence
Acoustic and core data from Cumberland Sound show that glacial ice derived from the Foxe Sector (Amadjuak Dome) of the Laurentide Ice Sheet advanced to the continental shelf at the mouth of the sound during a late phase of the Foxe Glaciation. The basal lithofacies/acoustic unit (Ai/BUD) in the soun...
Published in: | Géographie physique et Quaternaire |
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Format: | Text |
Language: | English |
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Les Presses de l'Université de Montréal
1993
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Online Access: | http://id.erudit.org/iderudit/032929ar https://doi.org/10.7202/032929ar |