Overflow Glacier
Encyclopedia
Overflow Glacier is a steep tributary 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...

 spilling into Ferrar Glacier
Ferrar Glacier
The Ferrar Glacier is an Antarctic glacier about long, flowing from the plateau of Victoria Land west of the Royal Society Range to New Harbour in McMurdo Sound. The glacier makes a right turn northeast of Knobhead, where it is apposed, i.e., joined in Siamese-twin fashion, to Taylor Glacier...

 from the south, just east of Briggs Hill
Briggs Hill
Briggs Hill is a conspicuous ice-free hill, high, standing on the south side of Ferrar Glacier between Descent Glacier and Overflow Glacier in Victoria Land. It was charted by the British Antarctic Expedition, 1910–13, under Scott, and named by the Advisory Committee on Antarctic Names for...

, in Victoria Land
Victoria Land
Victoria Land is a region of Antarctica bounded on the east by the Ross Ice Shelf and the Ross Sea and on the west by Oates Land and Wilkes Land. It was discovered by Captain James Clark Ross in January 1841 and named after the UK's Queen Victoria...

. Given this descriptive name by the Western Journey Party, led by Taylor, of the British Antarctic Expedition, 1910-13.
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