Tsentral'naya Hill ( 70°45′S11°40′E / 70.750°S 11.667°E ; Russian : Гора Централная, romanized: Gora Tsentralnaya) is a bare rock hill (205 m) in the central part of the Schirmacher Hills, Queen Maud Land. The feature was mapped by the Soviet Antarctic Expedition in 1961 and named Gora Tsentral'naya (central hill).
This article incorporates public domain material from "Tsentral'naya Hill". Geographic Names Information System . United States Geological Survey.
The Beardmore Glacier in Antarctica is one of the largest valley glaciers in the world, being 200 km (125 mi) long and having a width of 40 km (25 mi). It descends about 2,200 m (7,200 ft) from the Antarctic Plateau to the Ross Ice Shelf and is bordered by the Commonwealth Range of the Queen Maud Mountains on the eastern side and the Queen Alexandra Range of the Central Transantarctic Mountains on the western. Its mouth is east of the Lennox-King Glacier. It is northwest of the Ramsey Glacier.
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.
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 Taylor Glacier is a glacier in Antarctica about 35 nautical miles long, flowing from the plateau of Victoria Land into the western end of Taylor Valley, north of the Kukri Hills. It flows to the south of the Asgard Range. The middle part of the glacier is bounded on the north by the Inland Forts and on the south by Beacon Valley.
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.
Foundation Ice Stream is a major ice stream in the Pensacola Mountains of Antarctica. The ice stream drains northward for 150 nautical miles along the west side of the Patuxent Range and the Neptune Range to enter the Ronne Ice Shelf westward of Dufek Massif.
Hut Point Peninsula is a long, narrow peninsula from 2 to 3 nautical miles wide and 15 nautical miles long, projecting south-west from the slopes of Mount Erebus on Ross Island, Antarctica. McMurdo Station (US) and Scott Base (NZ) are Antarctic research stations located on the Hut Point Peninsula.
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.
Explorers Range is a large mountain range in the Bowers Mountains of Victoria Land, Antarctica, extending from Mount Bruce in the north to Carryer Glacier and McLin Glacier in the south.
Ob' Bay is a bay lying between Lunik Point and Cape Williams in Antarctica. Lillie Glacier Tongue occupies the east part of the bay. The bay was charted by the Soviet Antarctic Expedition (1958) and named after the expedition ship Ob'.
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.
Rennick Glacier is broad glacier, nearly 200 nautical miles long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is 20 to 30 nautical miles wide, narrowing to 10 nautical miles near the coast. It takes its name from Rennick Bay where the glacier reaches the sea.
On the continent of Antarctica, the Aramis Range is the third range south in the Prince Charles Mountains, situated 11 miles southeast of the Porthos Range and extending for about 30 miles in a southwest–northeast direction. It was first visited in January 1957 by Australian National Antarctic Research Expeditions (ANARE) southern party led by W.G. Bewsher, who named it for a character in Alexandre Dumas' novel The Three Musketeers, the most popular book read on the southern journey.
Schirmacher Hills is a line of low coastal hills, 11 nautical miles (20 km) long, with numerous meltwater ponds, standing 40 nautical miles (70 km) north of the Humboldt Mountains along the coast of Queen Maud Land. Discovered by the Third German Antarctic Expedition under Alfred Ritscher, 1938–39, and named for Richardheinrich Schirmacher, pilot of the Boreas, one of the expedition seaplanes.
Dlinnoye Lake is a narrow, serpentine lake, 0.5 nautical miles (1 km) long, lying close northwest of Tsentral'naya Hill in the Schirmacher Hills, Queen Maud Land. The feature was mapped by the Soviet Antarctic Expedition in 1961 and named "Ozero Dlinnoye".
The Eland Mountains are a range of mountains which rise above 2,440 metres (8,010 ft) and extend about 20 nautical miles in a northeast–southwest direction along the south side of Clifford Glacier, on the east coast of Palmer Land, Antarctica.
Schanz Glacier is a glacier 8 nautical miles long in the Heritage Range, draining south between Soholt Peaks and Collier Hills to enter Union Glacier. It was mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos in 1961 to 1966. It was named by Advisory Committee on Antarctic Names (US-ACAN) for Lieutenant Commander Thomas L. Schanz, supply officer with U.S. Navy Squadron VX-6 during Deep Freeze in 1965.
Schirmacher Ponds is a group of meltwater ponds scattered among the Schirmacher Hills, lying 40 nautical miles (70 km) north of the Humboldt Mountains, along the coast of Queen Maud Land. Discovered by the German Antarctic Expedition under Ritscher, 1938–39, and named for Richardheinrich Schirmacher, pilot of the Boreas, one of the expedition seaplanes.
The Tomilin Glacier is a glacier over 15 nautical miles long, draining north from Pope Mountain in the central Wilson Hills. It enters the sea east of Goodman Hills and Cape Kinsey, forming a substantial glacier tongue.
