Pattern of Ice Surface Lowering for Rennick Glacier, Northern Victoria Land, Antarctica

Abstract Rennick Glacier is one of the major ice drainages in northern Victoria Land. Unlike glaciers farther south along the Transantarctic Mountains, Rennick Glacier does not drain into the Ross Ice Shelf but flows directly into a seasonally ice-covered ocean. Therefore, current fluctuations of th...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Mayewski, Paul A., Attig, John W., Drewry, David J.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000014052
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014052