The Miller Range is a mountain range extending south from Nimrod Glacier for 80 km (50 mi) along the western edge of the Marsh Glacier in Antarctica.
Skelton Glacier is a large glacier flowing from the polar plateau into the Ross Ice Shelf at Skelton Inlet on the Hillary Coast, south of Victoria Land, Antarctica.
The Wisconsin Range is a major mountain range of the Horlick Mountains in Antarctica, comprising the Wisconsin Plateau and numerous glaciers, ridges and peaks bounded by the Reedy Glacier, Shimizu Ice Stream, Horlick Ice Stream and the interior ice plateau.
Shackleton Glacier is a major Antarctic glacier, over 60 nautical miles long and from 5 to 10 nautical miles wide, descending from the Antarctic Plateau from the vicinity of Roberts Massif and flowing north through the Queen Maud Mountains to enter the Ross Ice Shelf between Mount Speed and Waldron Spurs. Discovered by the United States Antarctic Service (USAS) (1939–41) and named by the Advisory Committee on Antarctic Names (US-ACAN) for Sir Ernest Shackleton, British Antarctic explorer.
The Prince Olav Mountains is a mountain group in the Queen Maud Mountains in Antarctica stretching from Shackleton Glacier to Liv Glacier at the head of the Ross Ice Shelf.
The Deep Freeze Range is a rugged mountain range, over 80 nautical miles long and about 10 nautical miles wide, rising between Priestley and Campbell Glaciers in Victoria Land, Antarctica, and extending from the edge of the polar plateau to Terra Nova Bay. It is southwest of the Southern Cross Mountains, south of the Mesa Range and northeast of the Eisenhower Range of the Prince Albert Mountains.
Bowers Mountains is a group of north–south trending mountains in Antarctica, about 90 nautical miles long and 35 nautical miles wide, bounded by the coast on the north and by the Rennick Glacier, Canham Glacier, Black Glacier and Lillie Glacier in other quadrants. They are west of the Usarp Mountains, north of the Freyberg Mountains, northeast of the Concord Mountains, east of the Anare Mountains.
The David Glacier is a glacier over 60 nautical miles long, flowing east from the polar plateau through the Prince Albert Mountains to the coast of Victoria Land, Antarctica. It enters Ross Sea between Cape Philippi and Cape Reynolds to form the floating Drygalski Ice Tongue. It is the most imposing outlet glacier in Victoria Land. It is fed by two main flows which drain an area larger than 200,000 square kilometres, with an estimated ice discharge rate of 7.8 +/- 0.7 km3/year. The David Glacier was discovered by Ernest Shackleton's "Northern Party," in November 1908, under the leadership of Prof. T.W. Edgeworth David, of Sydney University, for whom the feature was named.
Crean Glacier is a glacier 4 miles (6.4 km) long, flowing northwest from Wilckens Peaks to the head of Antarctic Bay on the north coast of South Georgia. It was surveyed by the South Georgia Survey in the period 1951–57 and named by the UK Antarctic Place-Names Committee for Irishman Tom Crean, Second Officer of the Endurance during the British expedition under Ernest Shackleton, 1914–16. Crean accompanied Shackleton and Frank Worsley in the James Caird from Elephant Island to King Haakon Bay, South Georgia, and made the overland crossing with them to Stromness; this glacier lies on the route.
The Hays Mountains are a large group of mountains and peaks of the Queen Maud Mountains of Antarctica, surmounting the divide between the lower portions of Amundsen Glacier and Scott Glacier and extending from the vicinity of Mount Thorne on the northwest to Mount Dietz on the southeast.
Liv Glacier is a steep valley glacier, 40 nautical miles long, emerging from the Antarctic Plateau just southeast of Barnum Peak and draining north through the Queen Maud Mountains to enter Ross Ice Shelf between Mayer Crags and Duncan Mountains. It was discovered in 1911 by Roald Amundsen, who named it for the daughter of Fridtjof Nansen.
Zigzag Pass is a pass through the west portion of Wilckens Peaks in South Georgia, leading from Kohl Plateau to the head of Esmark Glacier. Descriptively named by United Kingdom Antarctic Place-Names Committee (UK-APC) in 1982 from the zigzag folding of the rocks in the pass.
Aitkenhead Glacier is a 10 nautical miles long glacier flowing east-southeast from the Detroit Plateau, Graham Land, into Prince Gustav Channel.
The Land Glacier is a broad, heavily crevassed glacier, about 35 nautical miles long, descending into Land Bay in Marie Byrd Land, Antarctica. It was discovered by the United States Antarctic Service (1939–41) and named for Rear Admiral Emory S. Land, Chairman of the United States Maritime Commission.
The Gothic Mountains is a group of mountains, 20 nautical miles long, in the Queen Maud Mountains of Antarctica, located west of Watson Escarpment and bounded by Scott Glacier, Albanus Glacier, and Griffith Glacier.
The Cathedral Rocks are a series of four abrupt cliffs interspersed by short glaciers and surmounted by sharp peaks. The cliffs extend for 8 nautical miles along the south side of Ferrar Glacier and form part of the north shoulder of the Royal Society Range, in Victoria Land, Antarctica.
Watson Escarpment is a major escarpment in the Queen Maud Mountains, trending northward along the east margin of Scott Glacier, then eastward to Reedy Glacier where it turns southward along the glacier's west side. Somewhat arcuate, the escarpment is nearly 100 nautical miles long, rises 3,550 metres (11,650 ft) above sea level, and 1,000 to 1,500 metres above the adjacent terrain.
Hobbs Ridge is a prominent arc-shaped ridge which circumscribes Hobbs Glacier to the north and northwest and forms the divide with the lower part of Blue Glacier, on the Scott Coast of Victoria Land, Antarctica. It was named in association with Hobbs Glacier. It forms the northernmost part of the Denton Hills.
Ramsey Glacier is a glacier about 45 nautical miles long in Antarctica. It originates in the Bush Mountains near the edge of the polar plateau and flows north through the Queen Maud Mountains of Antarctica to the Ross Ice Shelf eastward of Den Hartog Peak.
Robb Glacier is a glacier about 40 nautical miles (70 km) long that flows through the Ross Dependency to enter the west coast of the Ross Ice Shelf in Antarctica.
This article incorporates public domain material from "Wilckens Peaks". Geographic Names Information System . United States Geological Survey. 
