Dawson-Lambton Glacier
Encyclopedia
Dawson-Lambton Glacier is a heavily-crevassed glacier
Glacier
A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight...

 entering southeastern Weddell Sea
Weddell Sea
The Weddell Sea is part of the Southern Ocean and contains the Weddell Gyre. Its land boundaries are defined by the bay formed from the coasts of Coats Land and the Antarctic Peninsula. The easternmost point is Cape Norvegia at Princess Martha Coast, Queen Maud Land. To the east of Cape Norvegia is...

 immediately west of Brunt Ice Shelf
Brunt Ice Shelf
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...

. Discovered in January 1915 by a British expedition led by Schackleton. He named it for Elizabeth Dawson-Lambton, benefactress of the Shackleton expeditions.
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