Fiord to Deep Sea Sediment Transfers along the Northeastern Canadian Continental Margin: Models and Data
In Alaskan fiords, sedimentation rates are high; during a glacial advance fiord-basin sediments are transported to the ice front to form a shoal which reduces the calving rate. Thus, during successive glacial cycles, sediment is initially stored and then removed from fiord basins. In the fiords of e...
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
1990
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Online Access: | http://id.erudit.org/iderudit/032798ar https://doi.org/10.7202/032798ar |