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A correlation of the Tasmanian Pleistocene glacial epochs and deposits
Lewis, Arndell Neil (1933) A correlation of the Tasmanian Pleistocene glacial epochs and deposits. Papers and Proceedings of the Royal Society of Tasmania. pp. 67-76. ISSN 0080-4703
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The widespread range of Pleistocene glacial drifts in Tasmania was recognised by Charles Gould as early as 1860, and by 1885 R. M. Johnston had recorded their existence over the whole of the western highlands (Johnston, 1893). Until l893 no suggestion had been made that there had been more than one glacial phase in Tasmania, but in the paper last referred to R. M. Johnston recorded difficulties in the interpretation of the field evidence, which have since been used to prove the existence of such separate phases.
|Keywords:||Royal Society of Tasmania, RST, Van Diemens Land, natural history, science, ecology, taxonomy, botany, zoology, geology, geography, papers & proceedings, Australia, UTAS Library|
|Journal or Publication Title:||Papers and Proceedings of the Royal Society of Tasmania|
|Page Range:||pp. 67-76|
|Collections:||Royal Society Collection > Papers & Proceedings of the Royal Society of Tasmania|
|Additional Information:||Copyright Royal Society of Tasmania|
|Date Deposited:||12 May 2012 00:55|
|Last Modified:||18 Nov 2014 04:31|
|Item Statistics:||View statistics for this item|
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