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]

See also


  1. ^ "Mill Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2013-09-25.

Public Domain This article incorporates public domain material from the United States Geological Survey document: "Mill Glacier". (content from the Geographic Names Information System)

Coordinates: 85°10′S 168°30′E / 85.167°S 168.500°E / -85.167; 168.500