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...

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Bibliographic Details
Published in:Géographie physique et Quaternaire
Main Author: Andrews, John T.
Format: Text
Language:English
Published: Les Presses de l'Université de Montréal 1990
Subjects:
Online Access:http://id.erudit.org/iderudit/032798ar
https://doi.org/10.7202/032798ar