Authors / CoAuthors
Colhoun, E.A.
Abstract
A review, mainly of East Antarctic late Cainozoic (post 40 Ma) geological and geomorphological evidence, supports the hypothesis of the continuous presence of an ice sheet, of about the present size, since the late Miocene. Evidence is presented and the view advanced that, during the late Wisconsin maximum of isotope stage 2, ice was not nearly as thick or extensive over the continental shelf as required by the model of maximum Antarctic glaciation, Some of the factors influencing the contribution of Antarctica to post-glacial sea-level rise are discussed. It is considered that Antarcticas contribution was probably considerably less than previously estimated.
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document
eCat Id
81557
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Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
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Keywords
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- GA PublicationJournal
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- AAT
- Australian and New Zealand Standard Research Classification (ANZSRC)
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- Earth Sciences
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- Published_External
Publication Date
2000-01-01T00:00:00
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geoscientificInformation
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AGSO Journal of Australian Geology and Geophysics 17:5-6:121-131
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