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The Nimrod Glacier is a major glacier about 135 km (85 mi) long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains into the Ross Ice Shelf, Antarctica.
The Byrd Glacier is a major glacier in Antarctica, about 136 km (85 mi) long and 24 km (15 mi) wide. It drains an extensive area of the Antarctic plateau, and flows eastward to discharge into the Ross Ice Shelf.
The Churchill Mountains are a mountain range group of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica. They border on the western side of the Ross Ice Shelf, between Byrd Glacier and Nimrod Glacier.
The Deep Freeze Range is a rugged mountain range, over 128 km (80 mi) long and about 16 km (10 mi) wide, rising between Priestley and Campbell Glaciers in Victoria Land, Antarctica, and extending from the edge of the polar plateau to Terra Nova Bay. Peaks in the low and mid portions of the range were observed by early British expeditions to the Ross Sea.
Gair Glacier is a tributary glacier, 10 nautical miles long, rising close southeast of Mount Supernal in the Mountaineer Range and flowing east-northeast to enter Mariner Glacier just north of Bunker Bluff in Victoria Land, Antarctica. It was named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) 1962–63, for geologist H.S. Gair, leader that season of the NZGSAE northern field party.
Surveyors Range is a 30 miles (48 km) long mountain range in the Churchill Mountains of 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. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for the northern party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963–64, whose members carried out a topographical and geological survey of the area. The names of several party members are assigned to features in and about this range. All of the geographical features listed below lie situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Herz Glacier is a glacier flowing southeast from the vicinity of Mount Paterson to the east coast of South Georgia. It was named by the Second German Antarctic Expedition under Wilhelm Filchner, 1911–12.
The Alley Glacier is a glacier in Antarctica that drains the north slopes of Britannia Range in the vicinity of Ward Tower and flows north to Darwin Glacier. It is separated from Gaussiran Glacier by a series of large rock buttresses, including Robertson Buttress.
Beck Peak is a peak, 2,650 metres (8,700 ft) high, on the east flank of Amundsen Glacier, standing 2 nautical miles (4 km) northwest of Mount Stubberud on the ridge descending from the northern Nilsen Plateau, Queen Maud Mountains. This peak appears to have been first mapped from air and ground photos taken by the Byrd Antarctic Expedition, 1928–30. It was mapped in greater detail by the United States Geological Survey from surveys and from U.S. Navy air photos, 1960–64. The peak was named by the Advisory Committee on Antarctic Names for Andreas Beck, a crew member and ice pilot on Amundsen's South Pole expedition of 1910–12. This naming preserves the spirit of Roald Amundsen's 1911 commemoration of "Mount A. Beck", a name applied by him for a mountain situated at 87°20′S148°0′E.
The Gothic Mountains is a group of mountains, 32 kilometres (20 mi) long, in the Queen Maud Mountains of Antarctica, located west of Watson Escarpment and bounded by Scott Glacier, Albanus Glacier, and Griffith Glacier. The mountains were first visited in December 1934 by the Byrd Antarctic Expedition (ByrdAE) geological party led by Quin Blackburn. The name was proposed by Edmund Stump, leader of a U.S. Antarctic Research Program (USARP) - Arizona State University geological party which made investigations here in the 1980-81 season. The mountains are composed of granites which have weathered to produce a series of spires and peaks reminiscent of a Gothic cathedral.
The Carlstrom Foothills are a group of peaks and ridges in the Churchill Mountains, Antarctica.
Cooper Snowfield is a snowfield with an area of about 25 square miles (65 km2) in the Churchill Mountains of Antarctica.
Guerrero Glacier is a glacier about 7 nautical miles (13 km) long in Doyran Heights, draining from the southeast slopes of Mount Havener southwest of Beloslav Peak to the south side of Taylor Spur, in the southeast part of the Sentinel Range, Ellsworth Mountains, Antarctica. It was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1957–59, and was named by the Advisory Committee on Antarctic Names for John F. Guerrero, a meteorologist at South Pole Station in 1957.
Plummer Glacier is a short glacier descending east through the Enterprise Hills to the north of Lippert Peak and the Douglas Peaks, in the Heritage Range in Antarctica. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1961–66. Named by Advisory Committee on Antarctic Names (US-ACAN) for Charles C. Plummer, United States Antarctic Research Program (USARP) glaciologist at Palmer Station in 1965.
Lowe Glacier is a tributary glacier 7 nautical miles (13 km) long in the Queen Elizabeth Range, Antarctica. It flows south from a common saddle with the Prince of Wales Glacier 3 nautical miles (6 km) east of Mount Gregory to join the Princess Anne Glacier. The name was proposed by the Holyoake, Cobham and Queen Elizabeth Ranges Party of the New Zealand Geological Survey Antarctic Expedition, 1964–65, after D. Lowe, a member of the party.
Hurley Glacier is a glacier between Mount Gaudry and Mount Liotard, flowing east into Ryder Bay, Adelaide Island, Antarctica. It was named by the UK Antarctic Place-Names Committee in 1977 after Alec J. Hurley, a British Antarctic Survey mechanic at Halley Station, 1975–76, and Rothera Station, 1976–77.
Holyoake Range is a mountain range in the Ross Dependency of Antarctice. It is in the southern section of the Churchill Mountains, part of the Transantarctic Mountains System.
Hough Glacier is a glacier in central Doyran Heights in the Sentinel Range of Ellsworth Mountains, Antarctica, rising just south of Mount Tuck and flowing east-southeast for 10 nautical miles between Guerrero Glacier and Remington Glacier. It was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1957–59, and was named by the Advisory Committee on Antarctic Names for William S. Hough, who made ionosphere studies at South Pole Station in 1957.
The Kent Plateau is an ice-covered plateau in the northern extreme of the Churchill Mountains of Antarctica.
References
- ↑ "Gutenberg Glacier". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2012-05-11.
This article incorporates public domain material from "Gutenberg Glacier". Geographic Names Information System . United States Geological Survey.
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