Mill Glacier

Just upstream of Plunket Point, where it joins the Beardmore, there is an area of smooth and level blue ice over 7 kilometres (4.3 mi) long in a NNW-SSE direction that is suitable for an airfield.

Extensive icefalls near the head of Mill Glacier, between Otway Massif and the south part of Dominion Range.

An east-flowing glacier, 6 nautical miles (11 km; 6.9 mi) long, draining the east-central portion of the Dominion Range icecap.

Named by US-ACAN for Charles H. Vandament, USARP ionospheric physicist at South Pole Station in 1962.

An east-flowing glacier, 7 nautical miles (13 km; 8.1 mi) long, draining the east-central portion of the Dominion Range icecap.

Named by US-ACAN for Raymond J. Koski, USARP engineer on several traverses originating at the South Pole Station 1962-63, 1963–64 and 1964–65.

Southern head of the glacier (northwest corner of map)