Brunt Ice Shelf

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The Brunt Ice Shelf borders the Antarctic coast of Coats Land between Dawson-Lambton Glacier and Stancomb-Wills Glacier Tongue. It was the location of the base of the Royal Society Expedition, 1955-59 which was taken over as the British Halley Research Station.

Named by UK-APC after David Brunt, English meteorologist, Physical Secretary of the Royal Society, 1948-57, who was responsible for the initiation of the Royal Society Expedition to this ice shelf in 1955.

The Brunt Basin (75°0′S 25°0′W / -75, -25) is a glacially eroded basin of the Brunt Ice Shelf and partially of the Stancomb-Willis Glacier.

The Brunt Icefalls (75°55′S 25°0′W / -75.917, -25) extend along Caird Coast for about 80 km (50 mi), where the steep ice-covered coast descends to Brunt Ice Shelf. The icefalls were discovered November 5, 1967, in the course of a USN Squadron VXE-6 flight over the coast in LC-130 aircraft, and was plotted by United States Geological Survey from air photos obtained at that time. Named by US-ACAN in association with the Brunt Ice Shelf.

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This article incorporates text from Brunt Ice Shelf, in the Geographic Names Information System, operated by the United States Geological Survey, and therefore a public domain work of the United States Government. Coordinates: 75°40′S 025°00′W / -75.667, -25

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