Late Quaternary Ice-Surface Fluctuations of Beardmore Glacier, Transantarctic Mountains
Abstract Former longitudinal profiles of Beardmore Glacier, an outlet through the Transantarctic Mountains, constrain polar plateau elevations near the center of Antarctica and ice-shelf grouding in the southern Ross Embayment. Three gravel drift sheets of late Quaternary age occur alongside Beardmo...
Published in: | Quaternary Research |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1989
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Subjects: | |
Online Access: | http://dx.doi.org/10.1016/0033-5894(89)90005-7 http://api.elsevier.com/content/article/PII:0033589489900057?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589489900057?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400019633 |