Present and postglacial rates of uplift for glaciated northern and eastern North America derived from postglacial uplift curves

Average rates of postglacial uplift reach a maximum value of nearly 4 m 100 y −1 over southeastern Hudson Bay, and another high cell, with rates of about 2.5 m 100 y −1 , lies between Bathurst Inlet and Southampton Island. Current rates of uplift are underestimated if exponential curves are fitted s...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Author: Andrews, J. T.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1970
Subjects:
Online Access:http://dx.doi.org/10.1139/e70-069
http://www.nrcresearchpress.com/doi/pdf/10.1139/e70-069