Mill Glacier
Encyclopedia
Mill Glacier is a 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...

, 16 km wide, flowing northwest between the Dominion Range
Dominion Range
The Dominion Range is a broad mountain range, about long, forming a prominent salient at the juncture of the Beardmore and Mill glaciers in Antarctica. The range is part of the Queen Maud Mountains...

 and the Supporters Range
Supporters Range
The Supporters Range is a rugged range of mountains in Antarctica, 40 km long, bordering the eastern side of Mill Glacier, from Keltie Glacier in the north to Mill Stream Glacier in the south....

 into Beardmore Glacier
Beardmore Glacier
The Beardmore Glacier in Antarctica is one of the largest glaciers in the world, with a length exceeding 160 km . The glacier is one of the main passages from the Ross Ice Shelf through the Queen Alexandra and Commonwealth ranges of the Transantarctic Mountains to the Antarctic Plateau, and was one...

. Discovered by the British Antarctic Expedition (1907-09) and named for Hugh Robert Mill
Hugh Robert Mill
Hugh Robert Mill was a Scottish geographer and meteorologist who was influential in the reform of geography teaching, and in the development of meteorology as a science. Educated in Scotland, he graduated from the University of Edinburgh in 1883...

, British geographer and Antarctic historian.

See also

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