Related Research Articles
The Nimrod Glacier is a major glacier about 85 nautical miles long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains into the Ross Ice Shelf, Antarctica.
The Dennistoun Glacier is a glacier, 50 nautical miles long, draining the northern slopes of Mount Black Prince, Mount Royalist and Mount Adam in the Admiralty Mountains of Victoria Land, Antarctica. It flows northwest between the Lyttelton Range and Dunedin Range, turning east on rounding the latter range to enter the sea south of Cape Scott.
The Tapley Mountains is a range of mountains fronting on the eastern side of the Scott Glacier, extending eastward for 35 nautical miles between Leverett Glacier and Albanus Glacier in the Queen Maud Mountains of Antarctica.
The Amundsen Glacier is a major Antarctic glacier, about 7 to 11 km wide and 150 km (80 nmi) long. It originates on the Antarctic Plateau where it drains the area to the south and west of Nilsen Plateau, then descends through the Queen Maud Mountains to enter the Ross Ice Shelf just west of the MacDonald Nunataks.
The Priestley Glacier is a major valley glacier, about 60 nautical miles long, originating at the edge of the Polar Plateau of Victoria Land, Antarctica. The glacier drains southeast between the Deep Freeze Range and Eisenhower Range to enter the northern end of the Nansen Ice Sheet. It was first explored by the Northern Party of the British Antarctic Expedition, 1910–13, and named for Raymond Priestley, a geologist with the Northern Party.
Lillie Glacier is a large glacier in Antarctica, about 100 nautical miles long and 10 nautical miles wide. It lies between the Bowers Mountains on the west and the Concord Mountains and Anare Mountains on the east, flowing to Ob' Bay on the coast and forming the Lillie Glacier Tongue.
Tucker Glacier is a major valley glacier of Victoria Land, Antarctica, about 90 nautical miles long, flowing southeast between the Admiralty Mountains and the Victory Mountains to the Ross Sea. There is a snow saddle at the glacier's head, just west of Homerun Range, from which the Ebbe Glacier flows northwestward.
The Scaife Mountains is a group of mountains rising west of Prehn Peninsula and between the Ketchum Glacier and Ueda Glacier, at the base of the Antarctic Peninsula.
Rongé Island is a high, rugged island 5 nautical miles long, the largest island of the group which forms the west side of Errera Channel, off the west coast of Graham Land in Antarctica.
The Prince Charles Mountains are a major group of mountains in Mac. Robertson Land in Antarctica, including the Athos Range, the Porthos Range, and the Aramis Range. The highest peak is Mount Menzies, with a height of 3,228 m (10,591 ft). Other prominent peaks are Mount Izabelle and Mount Stinear. These mountains, together with other scattered peaks, form an arc about 420 km (260 mi) long, extending from the vicinity of Mount Starlight in the north to Goodspeed Nunataks in the south.
The French Antarctic Expedition is any of several French expeditions in Antarctica.
Wilson Hills is a group of scattered hills, nunataks and ridges that extend northwest–southeast about 70 nautical miles between Matusevich Glacier and Pryor Glacier in Antarctica.
The Mariner Glacier is a major glacier over 60 nautical miles long, descending southeast from the plateau of Victoria Land, Antarctica, between Mountaineer Range and Malta Plateau, and terminating at Lady Newnes Bay, Ross Sea, where it forms the floating Mariner Glacier Tongue.
The Mountaineer Range is the range of mountains lying between the Mariner Glacier and Aviator Glacier in Victoria Land, Antarctica. It lies to the south of the Victory Mountains and northeast of the Southern Cross Mountains.
Altimir Glacier is a 4.8-kilometre (3.0 mi) long and 5.5-kilometre (3.4 mi) wide glacier draining the north slopes of the Osterrieth Range on Anvers Island in the Palmer Archipelago, Antarctica. It flows northwards to enter Dalchev Cove in Fournier Bay east of Studena Point.
Kleptuza Glacier is a 6 km long and 6 km wide glacier draining the east slopes of Mount Hector in the Trojan Range and the north slopes of Osterrieth Range on Anvers Island in the Palmer Archipelago, Antarctica. Situated southeast of Thamyris Glacier and west of Altimir Glacier. Flowing northwards to enter Fournier Bay east of Madzharovo Point and west of Studena Point.
Mount Camber is a mainly snow-covered mountain, 1,400 metres (4,600 ft) high, 1 nautical mile (2 km) northeast of Molar Peak in the Osterrieth Range of Anvers Island, in the Palmer Archipelago. It was first seen by the Belgian Antarctic Expedition, 1897–99, under Gerlache. The name High Peak was probably given to the feature by Lieutenant Commander J.M. Chaplin, Royal Navy, during a sketch survey in 1927 on the RRS Discovery. A resurvey in 1955 by the Falkland Islands Dependencies Survey found this descriptive name to be unsuitable. The new name, given by the UK Antarctic Place-Names Committee, is descriptive of the summit, which is long and gently sloping like a cambered road surface.
Campbell Glacier is a glacier, about 60 nautical miles long, originating near the south end of Mesa Range and draining southeast between the Deep Freeze Range and Mount Melbourne to discharge into north Terra Nova Bay in Victoria Land, Antarctica.
Molar Peak is a steep-sided peak, 1,065 metres (3,500 ft) high, between Mount Camber and Copper Peak in the Osterrieth Range of Anvers Island, in the Palmer Archipelago, Antarctica. It was named by the UK Antarctic Place-Names Committee following a survey by the Falkland Islands Dependencies Survey in 1955. The descriptive name arose because the peak is shaped like a tooth.
Copper Col is a col at 305 m, between Copper Peak and Billie Peak in the Osterrieth Range of Anvers Island, in the Palmer Archipelago. Probably first seen by the Belgian Antarctic Expedition (1897–99), under Adrien de Gerlache. The name Copper Glacier appears in this position on a chart based on a 1927 survey by Discovery Investigations personnel on the RRS Discovery. The feature was resurveyed in 1955 by the Falklands Islands Dependencies Survey, who reported that col would be a better descriptive term.
References
This article incorporates public domain material from "Osterrieth Range". Geographic Names Information System . United States Geological Survey.
 | This Anvers Island location article is a stub. You can help Wikipedia by expanding it. |