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