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...
Published in: | Quaternary Research |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
1988
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Online Access: | http://dx.doi.org/10.1016/0033-5894(88)90019-1 http://api.elsevier.com/content/article/PII:0033589488900191?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589488900191?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400019207 |