Pleistocene periglacial landforms are widespread in Australia and provide valuable information on past temperatures, but dating the time of their formation has proven difficult. To remedy this, we have explored the use of cosmogenic 36Cl for direct dating of periglacial deposits. We sampled six deposits in four locations in southeastern Australia, ranging from blockstreams and block slopes to former rock glaciers. Eighteen exposure ages reveal a concentration of periglacial activity during the last glacial maximum (LGM) between 16 and 23ka, with a population having a weighted mean age of 21.9±0.5ka. This age is shortly before the time of maximum ice advance during the LGM in southeastern Australia. Exposure dating of block deposits provides...
The Australian region spans some 60° of latitude and 50° of longitude and displays considerable regi...
The Australian region spans some 60° of latitude and 50° of longitude and displays considerable regi...
U–Pb dating and Hf-isotope provenance analysis of detrital zircons from the glaciogenic lower Permia...
Only a small area of the Australian mainland was glaciated during the Pleistocene, whereas periglaci...
Late Pleistocene glaciation of Australia was restricted to the Snowy Mountains and the Tasmanian hig...
Australia was glaciated several times during the Pleistocene and possibly during the Pliocene. On th...
2020 Elsevier Ltd The Quaternary is well known for being a period of the geological record that saw ...
Copyright © 2009 Elsevier Ltd All rights reserved.This study forms part of a wider investigation of ...
A high-resolution, multiproxy record encompassing the last glacial-interglacial transition is presen...
Many Tasmanian deposits previously described as 'periglacial' have been described in more detail, re...
Published online: 22 May 2013Alluvial-channel and overlying eolian deposits exposed in coastal cliff...
Quaternary alluvial sediments occur within and on the flanks of the Mt Lofty Ranges of southern Sout...
Moraines on Schnells Ridge, southwest Tasmania, have been dated using in situ 10Be. An age of 19,400...
A number of models, developed primarily in the 1980s, propose that Aboriginal Australian populations...
The development and application of geochronological tools suitable for dating Cenozoic rocks and pro...
The Australian region spans some 60° of latitude and 50° of longitude and displays considerable regi...
The Australian region spans some 60° of latitude and 50° of longitude and displays considerable regi...
U–Pb dating and Hf-isotope provenance analysis of detrital zircons from the glaciogenic lower Permia...
Only a small area of the Australian mainland was glaciated during the Pleistocene, whereas periglaci...
Late Pleistocene glaciation of Australia was restricted to the Snowy Mountains and the Tasmanian hig...
Australia was glaciated several times during the Pleistocene and possibly during the Pliocene. On th...
2020 Elsevier Ltd The Quaternary is well known for being a period of the geological record that saw ...
Copyright © 2009 Elsevier Ltd All rights reserved.This study forms part of a wider investigation of ...
A high-resolution, multiproxy record encompassing the last glacial-interglacial transition is presen...
Many Tasmanian deposits previously described as 'periglacial' have been described in more detail, re...
Published online: 22 May 2013Alluvial-channel and overlying eolian deposits exposed in coastal cliff...
Quaternary alluvial sediments occur within and on the flanks of the Mt Lofty Ranges of southern Sout...
Moraines on Schnells Ridge, southwest Tasmania, have been dated using in situ 10Be. An age of 19,400...
A number of models, developed primarily in the 1980s, propose that Aboriginal Australian populations...
The development and application of geochronological tools suitable for dating Cenozoic rocks and pro...
The Australian region spans some 60° of latitude and 50° of longitude and displays considerable regi...
The Australian region spans some 60° of latitude and 50° of longitude and displays considerable regi...
U–Pb dating and Hf-isotope provenance analysis of detrital zircons from the glaciogenic lower Permia...