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Underground drainage at Mole Creek, Tasmania

Bibliographic Data

ID8384416
AuthorsKevin Kiernan
Year1990
Volume28
Issue2
Pages224-239
Publication date1990-10-01
Open AccessYes
TypeARTICLE
VenueAustralian Geographical Studies (JOURNAL)
Journal identifiersISSN: 0004-9190 • E-ISSN: 1467-8470
PublisherWiley (PUBLISHER • GB)
DOI10.1111/j.1467-8470.1990.tb00614.x
OpenAlexW1985923548
LanguageEN
References cited4

Complex patterns of groundwater flow exist in the Mole Creek karst area, Tasmania. Many surface drainage divides are breached underground The evolution of the drainage has been dominated by (I) the deflection of streams along the strike of the limestone beds; (2) progressive changes to hydraulic gradients; and (3) a history of climate change during the Quaternary that has seen drainage diverted underground by glaciers and/or by proglacial and periglacial sedimentation

Aquifer · Drainage · Geochemistry · Geomorphology · Geotechnical engineering · Glacier · Groundwater · Groundwater flow · Hydrology (agriculture · Karst · Quaternary · Sediment · Sedimentation · STREAMS · Ecology · Geology · Groundwater and Watershed Analysis · Karst Systems and Hydrogeology · Landslides and related hazards · Paleontology

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  • Glacial Stratigraphy of the Upper Mersey Valley, Tasmania

    Open Access•D G HANNAN, D Hannan et al.•Australian Geographical Studies•1987

Highly citedNo

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