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Weathering evidence for an additional glacial stage in Tasmania

Bibliographic Data

ID8384558
AuthorsKevin Kiernan
Year1983
Volume21
Issue2
Pages197-220
Publication date1983-10-01
Open AccessYes
TypeARTICLE
VenueAustralian Geographical Studies (JOURNAL)
Journal identifiersISSN: 0004-9190 • E-ISSN: 1467-8470
PublisherWiley (PUBLISHER • GB)
DOI10.1111/j.1467-8470.1983.tb00444.x
OpenAlexW2097679283
LanguageEN
Citations received15
References cited41

Quantitative studies of relative dating parameters, including subsurface dolerite weathering rind thickness and weathering front penetration, permit the differentiation of three broad groupings of till deposits in several valleys in north‐central, western, western‐central and south‐western Tasmania. An early cold climatic phase – the Linda Glacial Stage– is recognised on the basis of this weathering evidence which also indicates that there have been at least two more recent Glacial Stages of decreasing severity, termed here the Henty and Margaret Glacial Stages respectively. This three‐fold model bears a striking similarity to that of Lewis (1945) which was rejected nearly three decades ago. However, whereas Lewis' model was founded upon erosional evidence, the present study is based entirely upon depositional and weathering evidence

Earth science · Geography · Geomorphology · Glacial period · Physical geography · Stage (stratigraphy · Weathering · Geological formations and processes · Geology · Geology and Paleoclimatology Research · Paleontology · Pleistocene-Era Hominins and Archaeology

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Citations per year0.38
Citation span1986 - 1999 (14)
Highly citedNo

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