Geological evidence for changes in the East Antarctica ice sheet (60°–120°E) during the last glaciation

Abstract The East Antarctica ice sheet advanced onto the continental shelf during the last glaciation but appears to have been thinner (<300 m) than previously hypothesised and probably did not everywhere extend to the edge of the continental shelf. Where the shelf is wide, the ice probably termi...

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Bibliographic Details
Published in:Polar Record
Main Author: Colhoun, Eric A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1991
Subjects:
Online Access:http://dx.doi.org/10.1017/s0032247400013103
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400013103