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Holocene landscape instability in the Dazzler Range, northern Tasmania

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Kiernan, K (1998) Holocene landscape instability in the Dazzler Range, northern Tasmania. Papers and Proceedings of the Royal Society of Tasmania, 132. pp. 35-40. ISSN 0080-4703

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Abstract

At least 5m of poorly consolidated Quaternary sediments have accumulated since the mid Holocene in the lower reaches of stream channels
that drain the flanks of the Dazzler Range. Radiocarbon assay of charcoal and wood fragments contained in the sediments indicate
deposition during the mid to late Holocene 5.2-1.8 ka. Coarse gravels in the earliest deposits are believed to have been recycled from relict
periglacial gravels in response to increased runoff and channel instability, brought about by neoglacial cooling coupled with changes in
vegetation structure and associated fire frequency. The thickness of the sediments and the presence oflarge logs in the sediments along
the lower reaches of Branchs Creek suggest at least one geomorphic event of high magnitude. Significant aggradation of finer calibre
sediments has continued during the last two millenia. Since European settlement, deep gulleys have formed in the lower reaches of alluvial
fans that flank the range, in response to land dearing for agriculture and the artificial straightening of stream channels. The earlier history
of slope instability and sediment aggradation, even under natural conditions, highlights the need for careful land management.

Item Type: Article
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. 35-40
ISSN: 0080-4703
Collections: Royal Society Collection > Papers & Proceedings of the Royal Society of Tasmania
Additional Information:

Copyright Royal Society of Tasmania

Date Deposited: 22 May 2012 02:49
Last Modified: 18 Nov 2014 04:33
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