Mill Glacier
Glacier in Antarctica / From Wikipedia, the free encyclopedia
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Not to be confused with Mills Glacier.
Mill Glacier (85°10′S 168°30′E) is a tributary glacier, 10 nautical miles (19 km) wide, flowing northwest between the Dominion Range and the Supporters Range into Beardmore Glacier, Antarctica. It was discovered by the British Antarctic Expedition, 1907–09, and named for Hugh Robert Mill, a British geographer and Antarctic historian.[1]