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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|
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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