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Glacial Crooked Lake, Vestfold Hills, East Antarctica

Published online by Cambridge University Press:  27 October 2009

D.B. Gore ,
J. Pickard ,
A.S. Baird  and
J.A. Webb
D.B. Gore
Affiliation:
Department of Geography, The University of Newcastle, Callaghan, NSW 2308, Australia
J. Pickard
Affiliation:
Graduate School of the Environment, acquarie University, NSW 2109, Australia
A.S. Baird
Affiliation:
Department of Geography, The University of Newcastle, Callaghan, NSW 2308, Australia
J.A. Webb
Affiliation:
Department of Geography, The University of Newcastle, Callaghan, NSW 2308, Australia
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Abstract

Glacial Crooked Lake was an ice-dammed impoundment in Vestfold Hills, East Antarctica, that had a volume of (250 ± 45) × 10 m. The impoundment is inferred to have existed during deglaciation following the Late Holocene Chelnok Advance of Sørsdal Glacier. The dam released water incrementally, allowing the formation of four major series of shorelines with a maximum height of 24 m above the current lake level of 22 m asl. Water from Glacial Crooked Lake overflowed into Watts Lake downstream, allowing saltwater there to mix, dilute, and be transported to the sea via Ellis Rapids. In this way water in Watts Lake became fresh, and alluvial fans consisting of cobbles and boulders formed below Crooked Lake and Ellis Rapids.

Type
Articles
Information
Polar Record , Volume 32 , Issue 180 , January 1996 , pp. 19 - 24
Copyright
Copyright © Cambridge University Press 1996

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References

Adamson, D.A., and Pickard, J.. 1986. Cainozoic history of the Vestfold Hills. In: Pickard, J. (editor). Antarctic oasis. Sydney: Academic Press: 63–97.Google Scholar
Blachut, S.P., and McCann, S.B.. 1981. The behaviour of a polar ice-dammed lake, Ellesmere Island, NWT, Canada. Arctic and Alpine Research 13: 63–74.CrossRefGoogle Scholar
Colhoun, E.A., and Adamson, D.A.. 1989. Former glacial lakes of the Bunger Hills, Antarctica. Australian Geographer 20: 125–135.CrossRefGoogle Scholar
Colhoun, E.A., and Adamson, D.A.. 1992. Raised beaches of the Bunger Hills, Antarctica. Canberra: Australian Government Publishing Service (ANARE Report 136).Google Scholar
Gore, D.B. 1992. Ice-damming and fluvial erosion in the Vestfold Hills, East Antarctica. Antarctic Science 4: 227–234.CrossRefGoogle Scholar
Gore, D.B. 1993. Changes in the ice boundary of the Vestfold Hills, East Antarctica, from 1947 to 1990. Australian Geographical Studies 31: 49–61.CrossRefGoogle Scholar
Gore, D.B. 1995. Geomorphological processes and Quaternary sediments of the Vestfold Hills, East Antarctica. Unpublished PhD thesis. Newcastle, Australia: The University of Newcastle.Google Scholar
Pickard, J., and Adamson, D.A.. 1983. Perennially frozen lakes at glacier/rock margins, East Antarctica. In: Oliver, R. L., James, P.R., and Jago, J.B. (editors). Antarctic Earth science. Canberra: Australian Academy of Science: 470–472.Google Scholar
Pickard, J., Adamson, D.A., and Heath, C.W.. 1986. The evolution of Watts Lake, Vestfold Hills, East Antarctica, from marine inlet to freshwater lake. Palaeogeography, Palaeoclimatology, Palaeoecology 53: 271–288.CrossRefGoogle Scholar
Sissons, J.B. 1978. The parallel roads of Glen Roy and adjacent glens, Scotland. Boreas 7: 229–244.CrossRefGoogle Scholar
Zhang, Q., and Peterson, J.A.. 1984. A geomorphology and Late Quaternary geology of the Vestfold Hills, Antarctica. Canberra: Australian Government Publishing Service (ANARE Report 133).Google Scholar