Late Quaternary glaciation and deglaciation of the Bunger Hills, Antarctica

The Bunger Hills were covered by the Antarctic Ice Sheet during the last glaciation. During deglaciation the ice sheet margin collapsed into the marine inlets and the sea entered the oasis before 7.7 ka BP. Raised beaches occur widely below 8.5 m and indicate uplift at 1.4 m ka −1 during the middle...

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Bibliographic Details
Published in:Antarctic Science
Main Authors: Adamson, Donald A., Colhoun, Eric A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1992
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102092000658
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102092000658