More on Deep Glacial Erosion by Continental Ice Sheets and Their Tongues of Distributary Ice

High latitude intracontinental seaways occupy great troughs carved by broad tongues of inland ice as it debouched to deep marine water. Such troughs occur in glaciated coasts, but not in stable, nonglaciated ones. Where ice flowed along the walls of troughs whose adjacent uplands held local glaciers...

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Bibliographic Details
Published in:Quaternary Research
Main Author: White, William A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1988
Subjects:
Online Access:http://dx.doi.org/10.1016/0033-5894(88)90019-1
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