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    <title>UTas ePrints - Cosmogenic nuclide ages for Last Glacial Maximum moraine at Schnells Ridge, Southwest Tasmania</title>
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    <meta content="Kiernan, Kevin" name="eprints.creators_name" />
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<meta content="Moraines on Schnells Ridge, southwest Tasmania, have been dated using in situ 10Be. An age of 19,400 F 600 yr is indicated for the wellpreserved
innermost moraine from consistent measurements on four large quartzite boulders. This corresponds closely with exposure ages
reported by T.T. Barrows et al. (2002, Quaternary Science Reviews 21, 159–173) for Last Glacial Maximum glacial features farther north in
Tasmania and southeast Australia. In contrast, ages between 39,000 and 141,000 yr were obtained from a series of boulders on a more
extensive outer moraine, indicating that this has had a more complex history." name="eprints.abstract" />
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Quaternary Research 55 (2), 179– 189.
Barrows, T.T., Stone, J.O., Fifield, L.K., Cresswell, R.G., 2002. The timing
of the Last Glacial Maximum in Australia. Quaternary Science Reviews
21, 159– 173.
Colhoun, E.A., 1985. Glaciations of the West Coast Range, Tasmania.
Quaternary Research 24, 39–59.
Fifield, L.K., 1999. Accelerator mass spectrometry and its applications.
Reports on Progress in Physics 62, 1223–1274.
Fifield, L.K., Ophel, T.R., Allan, G.L., Bird, J.R., Davie, R.F., 1990.
Accelerator mass spectrometry at the Australian National University’s
14UD accelerator: experience and developments. Nuclear Instruments
and Methods B52, 233–237.
Gosse, J.C., Stone, J.O., 2001. Terrestrial cosmogenic nuclide methods
passing milestones towards paleo-altimetry. EOS, Transactions of the
American Geophysical Union 82/7, 81– 89.
Kiernan, K., 1990. The alpine geomorphology of the Mt Anne massif,
southwestern Tasmania. Australian Geographer 21, 113– 125.
Kiernan, K., 1991. Glacial history of the upper Derwent Valley, Tasmania.
New Zealand Journal of Geology and Geophysics 34, 157– 166.
Kiernan, K., Lauritzen, S.-E., Duhig, N., 2001. Glaciation and cave sediment
aggradation around the margins of the Mt Field Plateau, Tasmania.
Australian Journal of Earth Sciences 48, 251–263.
Kohl, C.P., Nishiizumi, K., 1992. Chemical isolation of quartz for measurement
of in-situ-produced cosmogenic nuclides. Geochimica et Cosmochimica
Acta 56, 3583–3587.
Lal, D., 1991. Cosmic ray labeling of erosion surfaces: in situ nuclide
production rates and erosion models. Earth and Planetary Science Letters
104, 424–439.
Middleton, R., Klein, J., 1987. A new method for measuring 10Be/9Be
ratios. Philosophical Transactions of the Royal Society A323, 121– 123.
Williams, P.W., 1996. A 230 ka record of glacial and interglacial events
from Aurora Cave, Fiordland, New Zealand. New Zealand Journal of
Geology and Geophysics 39, 225–241." name="eprints.referencetext" />
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<meta content="Moraines on Schnells Ridge, southwest Tasmania, have been dated using in situ 10Be. An age of 19,400 F 600 yr is indicated for the wellpreserved
innermost moraine from consistent measurements on four large quartzite boulders. This corresponds closely with exposure ages
reported by T.T. Barrows et al. (2002, Quaternary Science Reviews 21, 159–173) for Last Glacial Maximum glacial features farther north in
Tasmania and southeast Australia. In contrast, ages between 39,000 and 141,000 yr were obtained from a series of boulders on a more
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    <h1 class="ep_tm_pagetitle">Cosmogenic nuclide ages for Last Glacial Maximum moraine at Schnells Ridge, Southwest Tasmania</h1>
    <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Kiernan, Kevin</span> and <span class="person_name">Fifield, L. Keith</span> and <span class="person_name">Chappell, John</span> (2004) <xhtml:em>Cosmogenic nuclide ages for Last Glacial Maximum moraine at Schnells Ridge, Southwest Tasmania.</xhtml:em> Quaternary Research, 61 . pp. 335-338. ISSN 1096-0287</p><p style="margin-bottom: 1em" class="not_ep_block"></p><table style="margin-bottom: 1em" class="not_ep_block"><tr><td valign="top" style="text-align:center"><a href="http://eprints.utas.edu.au/2352/1/Cosmogenicnuclide.pdf"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" class="ep_doc_icon" border="0" /></a></td><td valign="top"><a href="http://eprints.utas.edu.au/2352/1/Cosmogenicnuclide.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />356Kb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input accept-charset="utf-8" value="3009" name="docid" type="hidden" /><div class=""><input value="Request a copy" name="_action_null" class="ep_form_action_button" onclick="return EPJS_button_pushed( '_action_null' )" type="submit" /> </div></form></td></tr></table><p style="margin-bottom: 1em" class="not_ep_block">Official URL: <a href="http://dx.doi.org/10.1016/j.yqres.2004.02.004">http://dx.doi.org/10.1016/j.yqres.2004.02.004</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">Moraines on Schnells Ridge, southwest Tasmania, have been dated using in situ 10Be. An age of 19,400 F 600 yr is indicated for the wellpreserved&#13;
innermost moraine from consistent measurements on four large quartzite boulders. This corresponds closely with exposure ages&#13;
reported by T.T. Barrows et al. (2002, Quaternary Science Reviews 21, 159–173) for Last Glacial Maximum glacial features farther north in&#13;
Tasmania and southeast Australia. In contrast, ages between 39,000 and 141,000 yr were obtained from a series of boulders on a more&#13;
extensive outer moraine, indicating that this has had a more complex history.</p></div><table style="margin-bottom: 1em" cellpadding="3" class="not_ep_block" border="0"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Article</td></tr><tr><th valign="top" class="ep_row">Additional Information:</th><td valign="top" class="ep_row">The definitive version is available at http://www.sciencedirect.com&#13;
</td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">Glaciation; Tasmania; Cosmogenic nuclide dating</td></tr><tr><th valign="top" class="ep_row">Subjects:</th><td valign="top" class="ep_row"><a href="http://eprints.utas.edu.au/view/subjects/260000.html">260000 Earth Sciences</a><br /><a href="http://eprints.utas.edu.au/view/subjects/260100.html">260000 Earth Sciences &gt; 260100 Geology</a><br /><a href="http://eprints.utas.edu.au/view/subjects/260115.html">260000 Earth Sciences &gt; 260100 Geology &gt; 260115 Glaciology</a></td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">2352</td></tr><tr><th valign="top" class="ep_row">Deposited By:</th><td valign="top" class="ep_row"><span class="ep_name_citation"><span class="person_name">Scholarly Publications Librarian</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">29 Oct 2007 13:35</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">09 Jan 2008 02:30</td></tr><tr><th valign="top" class="ep_row">ePrint Statistics:</th><td valign="top" class="ep_row"><a target="ePrintStats" href="/es/index.php?action=show_detail_eprint;id=2352;">View statistics for this ePrint</a></td></tr></table><p align="right">Repository Staff Only: <a href="http://eprints.utas.edu.au/cgi/users/home?screen=EPrint::View&amp;eprintid=2352">item control page</a></p>
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