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Australian Antarctic Ice Thickness Measurements and Sastrugi Observations, Mac-Robertson Land, 1957–58*

Published online by Cambridge University Press:  27 October 2009

Extract

The principal field activity of the A.N.A.R.E. party at Mawson during the 1957–58 summer was the determination of ice thickness along a section of the Antarctic plateau. In previous years the summer expeditions inland had concentrated on the survey and geology of the Prince Charles Mountains, south-east of Mawson. While this programme was continued in 1957–58 as opportunity presented, and in fact air photography of the ranges almost completed, the main I.G.Y. field effort was directed towards seismic ice-depth determinations. These were the responsibility of the Bureau of Mineral Resources, and a seismologist was seconded to the Antarctic Division, together with equipment for the purpose.

The traverse made lay southwards from Mawson, following approximately the meridian 62° 08′ E. It was known from prior air reconnaissance that a south-westerly spur of the Prince Charles Mountains system cut across the route in the vicinity of lat. 73° to 74° S., but the exact location was unknown. The intention was to map this spur, then skirt it to the west and resume the seismic traverse southwards.

Type
Articles
Copyright
Copyright © Cambridge University Press 1959

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References

1Mellor, M.. Australian glaciological contributions in Antarctica, Preliminary report. Journal of Glaciology, Vol. 3, No. 24, 1958, p. 279–85.CrossRefGoogle Scholar
2Goodspeed, M. J.. Preliminary report on measurements of ice thickness on the Antarctic ice cap by seismic and gravimetric methods. Bureau of Mineral Resources Record, Geology and Geophysics. Canberra, No. 40, 1958 (unpublished).Google Scholar
3Ball, F. K.. The theory of strong katabatic winds, Australian Journal of Physics, Vol. 9, No. 3, 1956, p. 373–86.CrossRefGoogle Scholar
4Crohn, P. W.. The geology and glaciology of Mac-Robertson Land and adjoining portions of Australian Antarctic Territory. Bureau of Mineral Resources Bulletin, Geology and Geophysics. Canberra, No. 52 (in the Press).Google Scholar