[Location: Location_Category='CONTINENT', Location_Type='ANTARCTICA', Detailed_Location='DUNLOP ISLAND']
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Baseline information on both the modern processes operating on Antarctic beaches and the development of beach ridges in relation to the last glaciation ice retreat and isostatic rebound
Entry ID:
K043_1996_1998_NZ_1
Summary
Abstract:
Beaches in McMurdo Sound have developed since the last glaciation when ice sheets were at their maximum. The weight of the overlying ice, depressed the land, which has slowly rebounded forming a series of beaches. To obtain a height above sea level today, it is necessary to know where sea level was on the raised beach ridges. The process of modern beach formation was investigated to help determine ...
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The thesis and resulting publication is available online at the GET DATA link. Additional data is contained within a CD available with the original thesis. Please contact the investigator for more information.
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Publications/References
Butler, E.R.T. Process environments on modern and raised beaches in McMurdo Sound, Antarctica. Marine geology 162: 105-120, 1999.
Butler, E.R.T. Beaches in McMurdo Sound, Antarctica. Ph.D., Victoria University of Wellington, 2001. Creation and Review Dates
DIF Creation Date:
2005-09-22
Last DIF Revision Date:
2009-01-26
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