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.
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.
The Usarp Mountains are a major mountain range in North Victoria Land, Antarctica. They are west of the Rennick Glacier and trend north to south for about 190 kilometres (118 mi). The mountains are bounded to the north by Pryor Glacier and the Wilson Hills. They are west of the Bowers Mountains.
Lambert Glacier is a major glacier in East Antarctica. At about 80 km (50 mi) wide, over 400 km (250 mi) long, and about 2,500 m (8,200 ft) deep, it is the world's largest glacier. It drains 8% of the Antarctic ice sheet to the east and south of the Prince Charles Mountains and flows northward to the Amery Ice Shelf. It flows in part of Lambert Graben and exits the continent at Prydz Bay.
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 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.
Simpson Glacier is a glacier, 6 nautical miles, in the Admiralty Mountains, Antarctica. It flows northward to the coast between Nelson Cliff and Mount Cherry-Garrard where it forms the Simpson Glacier Tongue.
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.
The Latady Mountains are a group of mountains rising west of Gardner Inlet and between Wetmore Glacier and Ketchum Glacier, in southeastern Palmer Land, Antarctica.
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.
Krasheninnikov Peak is a peak, 2,525 metres (8,280 ft) high, on the south side of the Svarthausane Crags in the Südliche Petermann Range of the Wohlthat Mountains, Antarctica. It was discovered and plotted from air photos by the Third German Antarctic Expedition, 1938–39, and was mapped from air photos and surveys by the Sixth Norwegian Antarctic Expedition, 1956–60. It was remapped by the Soviet Antarctic Expedition, 1960–61, and named after Russian geographer S.P. Krasheninnikov.
Pitkevitch Glacier is a glacier, 20 nautical miles long, flowing north from the Admiralty Mountains along the west side of DuBridge Range in Antarctica. The glacier reaches the sea just east of Atkinson Cliffs, where it forms Anderson Icefalls. A portion of the terminus merges northwestward with Fendley Glacier.
The Eidshaugane Peaks are a group of peaks 1 nautical mile north of Eidsgavlen Cliff in the Humboldt Mountains of Queen Maud Land, Antarctica.
Gluck Peak is a rock peak, 335 metres (1,100 ft) high, located 6.5 nautical miles (12 km) south-southwest of Mount Borodin and immediately north of Alyabiev Glacier, lying between the bases of Bennett Dome and Shostakovich Peninsula on south side of the Beethoven Peninsula, southwest Alexander Island, Antarctica. It was first mapped from air photos taken by the Ronne Antarctic Research Expedition, 1947–48, by D. Searle of the Falkland Islands Dependencies Survey in 1960, and was named by the UK Antarctic Place-Names Committee after Christoph Willibald von Gluck, the Austrian composer (1714-1787).
Gråkammen Ridge is a mountainous ridge that includes Tambovskaya Peak and Mount Solov'yev, rising between the Gråhorna Peaks and Aurdalen Valley in the Westliche Petermann Range of the Wohlthat Mountains in Antarctica. It was discovered and plotted from air photos by the Third German Antarctic Expedition, 1938–39. It was replotted from air photos and surveys by the Sixth Norwegian Antarctic Expedition, 1956–60, and named Gråkammen.
Sandnesstaven Peak is a peak, 2,030 m, at the north end of the Conrad Mountains in the Orvin Mountains of Queen Maud Land. From 1956 to 1960, the Norwegian Antarctic Expedition mapped the peak using air photos and surveys and named it Sandnesstaven.
Salamander Range is a distinctive linear range between Canham Glacier and Black Glacier, in the Freyberg Mountains, Antarctica. The range was named by the Northern Party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963–64, from the nickname given to Lord Freyberg by Sir Winston Churchill, for the lizard that is untouched by fire.
Mount Solov'yev is a peak, 2,715 m, on the south part of Grakammen Ridge in Westliche Petermann Range, Wohlthat Mountains. Discovered and plotted from air photos by German Antarctic Expedition, 1938–39. Mapped from air photos and surveys by Norwegian Antarctic Expedition, 1956–60; remapped by Soviet Antarctic Expedition, 1960–61, and named after Soviet cartographer M.D. Solov'yev.
Holst Peak is a rocky pyramidal peak, rising to about 1,000 metres (3,300 ft), midway between the south end of the Walton Mountains and the LeMay Range in the central part of Alexander Island, Antarctica. It was first mapped by D. Searle of the Falkland Islands Dependencies Survey in 1960 from air photos obtained by the Ronne Antarctic Research Expedition, 1947–48, and was named by the UK Antarctic Place-Names Committee for Gustav Holst, the English composer.
This article incorporates public domain material from "Tambovskaya Peak". Geographic Names Information System . United States Geological Survey. 