Glacial history of the upper Derwent Valley, Tasmania.
Part of an extensive ice cap that developed in the Tasmanian Central Highlands during the late Cenozoic discharged southwards via a major outlet glacier that occupied the valley of the Derwent River. At least three and probably five phases of glaciation took place. The first and most extensive glaci...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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1991
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| Online Access: | https://eprints.utas.edu.au/10098/ https://eprints.utas.edu.au/10098/2/glacial_history.pdf http://www.royalsociety.org.nz/publications/journals/nzjg/1991/022/ |