Mill Glacier
Mill Glacier 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]
Not to be confused with Mills Glacier.
See also
References
This article incorporates public domain material from "Mill Glacier". Geographic Names Information System. United States Geological Survey.
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