Coastal Geomorphology, McMurdo Sound, Antarctica

Abstract Well-developed elevated beaches. deltaic deposits, marine-boulder pavements and wave-washed bedrock surfaces are found from Cape Bernacchi north to Granite Harbour. The highest measured marine feature, an elevated beach at Dunlop Island, is 20 m (67 ft) above sea-level. The highest beaches...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Nichols, Robert L.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1968
Subjects:
Earth-Surface Processes
McMurdo Sound
Cape Roberts
The Beaches
Wright Valley
Granite Harbour
Dunlop
Marble Point
Koettlitz Glacier
Bernacchi
Cape Bernacchi
Dunlop Island
Antarc*
Antarctica
Elephant Seal
Journal of Glaciology
Online Access:http://dx.doi.org/10.1017/s0022143000020657
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020657
Description
Summary:Abstract Well-developed elevated beaches. deltaic deposits, marine-boulder pavements and wave-washed bedrock surfaces are found from Cape Bernacchi north to Granite Harbour. The highest measured marine feature, an elevated beach at Dunlop Island, is 20 m (67 ft) above sea-level. The highest beaches at Marble Point and Cape Roberts, about 48 km (30 miles) apart, are about 20 m (66 ft) above sea-level. The marine limit between these two points is, therefore, essentially horizontal. The highest beach at Cape Bernacchi. approximately 4.8 km (3 miles) south of Marble Point, is about 12 m (40 ft) above sea-level, Well-developed elevated beaches disappear about 3.2 km (2 miles) south of Cape Bernacchi and are not found between this point and Koettlitz Glacier. These beaches post-date the youngest glaciation recognized in the lower Wright Valley. A 14 C analysis of an elephant seal buried in a 13 m (44 ft) beach at Marble Point indicates that this beach is 4450 ± 150 years old. As sea-level at this time was approximately 3 m (10 ft) lower than at present. the Marble Point area has risen isostatically about 16 m (54 ft) during the last 4450 ± 150 years. Pitted beaches, beaches deposited on ice, a buried elephant seal and gravel ridges deposited by ice indicate that all of the beaches were formed in a climate like that now found in the area.

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