The Dominion Range is a broad mountain range, about 48 km (30 mi) long, forming a prominent salient at the juncture of the Beardmore and Mill glaciers in Antarctica. The range is part of the Queen Maud Mountains
Shirase Glacier is a large glacier entering Havsbotn, the bay that forms the head of Lutzow-Holm Bay in Antarctica. The area occupied by this feature was first mapped as a bay and named Instefjorden by the Lars Christensen Expedition (LCE) of 1936-37. Surveys by Japanese Antarctic Research Expedition (JARE) of 1957-62, revealed the large glacier in this position which they named after Lt. Nobu Shirase, leader of the Japanese Antarctic Expedition of 1911-12.
Shanklin Glacier is a glacier in the Hughes Range of Antarctica, flowing southeast from Mount Waterman to enter Muck Glacier at a point 8 km (5 mi) west of Ramsey Glacier.
Icebreaker Glacier is a large valley glacier 10 miles (16 km) northeast of Mount Monteagle that flows southeast from the Mountaineer Range to Lady Newnes Bay, Victoria Land, Antarctica. Below Hermes Point its flow coalesces with that of Fitzgerald Glacier. The glacier was named by the New Zealand Geological Survey Antarctic Expedition, 1958–59, as a tribute to the work of the complements of U.S. Navy, and U.S. Coast Guard icebreakers in Antarctic exploration, in supporting scientists and in aiding other ships.
Anthony Glacier is a glacier which flows in an east-southeast direction to the east coast of Palmer Land where it terminates opposite the south tip of Hearst Island. The upper part of this glacier was seen by a sledge party of the British Graham Land Expedition under John Riddoch Rymill in 1936–37. The glacier was seen from the seaward side in 1940 by a sledging party from the East Base of the United States Antarctic Service, and in 1947 was photographed from the air by the Ronne Antarctic Research Expedition (RARE). It was named by Finn Ronne for Alexander Anthony of the J.P. Stevens Company, New York City, which contributed windproof clothing to the RARE.
Bader Glacier is a small glacier draining the west slopes of Rudozem Heights and flowing to Bourgeois Fjord just south of Thomson Head on German Peninsula, Fallières Coast on the west side of Graham Land, Antarctica.
Barrett Glacier is a glacier draining from the north slopes of the Prince Olav Mountains, about 15 nautical miles (30 km) long, flowing between the Longhorn Spurs and the Gabbro Hills to the Ross Ice Shelf. It was named by the Southern Party of the New Zealand Geological Survey Antarctic Expedition (1963–64) for Peter J. Barrett, a geologist with that party.
Cadman Glacier is a glacier, 1.5 nautical miles (3 km) wide at its mouth and about 7 nautical miles (13 km) long, flowing northwestward into the head of the southern arm of Beascochea Bay south of Plas Point on the west side of the Antarctic Peninsula.
Osicki Glacier is a narrow, deeply entrenched glacier just south of Mount Deakin in the Commonwealth Range, flowing west into Beardmore Glacier. Named by Advisory Committee on Antarctic Names (US-ACAN) for Kenneth J. Osicki, United States Antarctic Research Program (USARP) biologist at McMurdo Station, 1963.
Cunningham Glacier is a tributary glacier in the Queen Maud Mountains, flowing northeast to enter Canyon Glacier 5 nautical miles (9 km) north of Gray Peak. It was named by the Advisory Committee on Antarctic Names for Willard E. Cunningham, Jr., a cook at McMurdo Station, winter 1960, and at South Pole Station, winter 1963.
Swinford Glacier is a tributary glacier, 6 nautical miles (11 km) long, flowing southeast between Mount Holloway and Marshall Mountains to enter Beardmore Glacier. Discovered by the British Antarctic Expedition (1907–09) and named by Shackleton for his eldest son, Raymond Swinford. The map of the British Antarctic Expedition (1910–13) and some subsequent maps transpose the positions of Swinford Glacier and Berwick Glacier. The latter lies 12 nautical miles (22 km) northeastward. The original application of Berwick Glacier is the one recommended.
Gealy Spur is a high rock spur on the west side of Beardmore Glacier, Antarctica. The spur descends northeast from Mount Marshall and terminates in Willey Point. This area was first sighted by Ernest Shackleton's Southern Journey Party in December 1908. The spur was named by the Advisory Committee on Antarctic Names for William J. Gealy, a stratigrapher with the Ohio State University Geological Expedition of 1969–70, who worked the spur and found tetrapod fossils here.
Meridian Glacier is a broad glacier, 9 nautical miles (17 km) long, which flows south along the west side of Godfrey Upland and joins Clarke Glacier between Behaim Peak and Elton Hill, in southern Graham Land, Antarctica. Finn Ronne and Carl R. Eklund of the United States Antarctic Service travelled along this glacier in January 1941. It was photographed from the air by the Ronne Antarctic Research Expedition in November 1947, and was surveyed by the Falkland Islands Dependencies Survey in December 1958. The glacier was so named by the UK Antarctic Place-Names Committee because the glacier flows from north to south along the meridian.
Liotard Glacier is a channel glacier in Antarctica. It is about 3 nautical miles (6 km) wide and 6 nautical miles (11 km) long, and flows north-northeast from the continental ice, terminating in a small ice tongue about 4 nautical miles (7 km) west of Hélène Island. The glacier was delineated from air photos taken by U.S. Navy Operation Highjump, 1946–47, and was named by the Advisory Committee on Antarctic Names for Andre-Frank Liotard, the leader of the French Antarctic Expedition, 1949–51, whose group completed the initial survey of the coastal features as far westward as this glacier.
McMahon Glacier is a glacier about 18 nautical miles (33 km) long in the Anare Mountains of Victoria Land, Antarctica. It drains north between the Buskirk Bluffs and Gregory Bluffs into Nielsen Fjord. The glacier was named by the Antarctic Names Committee of Australia for F.P. McMahon, Logistics Officer with the Australian Antarctic Division, who led a number of expeditions to Macquarie Island and was second-in-charge of several expeditions to Antarctica.
The Marshall Mountains are a group of mountains overlooking Beardmore Glacier in the Queen Alexandra Range, Antarctica. They are bounded on the north by Berwick Glacier, and on the south by Swinford Glacier. The mountains were discovered by the South Polar Party of the British Antarctic Expedition (1907–09), and named for Dr. Eric Marshall, surgeon and cartographer to the expedition, a member of the Polar Party.
Hewson Glacier is a glacier in the Queen Alexandra Range, Antarctica, 15 nautical miles (28 km) long, flowing northeast to enter Beardmore Glacier just north of The Cloudmaker. It was named by the New Zealand Geological Survey Antarctic Expedition (1961–62) for Ronald Hewson, a surveyor with the expedition.
Snowy Point is a gently sloping point marking the north side of the western portal of Browning Pass in Deep Freeze Range, Victoria Land. First explored and given this descriptive name by the Northern Party of the British Antarctic Expedition, 1910-13.
Sowers Glacier is a glacier that flows from the prominent cirque on the east side of Craddock Massif and continues between Willis Ridge on the north, and Sanchez Peak and Stolnik Peak on the south, to join Thomas Glacier north of Mount Osborne, in the Sentinel Range, Ellsworth Mountains in Antarctica.
