Mount Jamroga ( 71°20′S163°6′E / 71.333°S 163.100°E Coordinates: 71°20′S163°6′E / 71.333°S 163.100°E ) is a mountain, 2,265 metres (7,430 ft) high, located 8 nautical miles (15 km) east of Mount Gow in the rugged heights between Carryer Glacier and Sledgers Glacier, in the Bowers Mountains of Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Lieutenant Commander John J. Jamroga, a photographic officer with the U.S. Naval Support Force in 1967 and 1968. [1] The topographical feature lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.
Mount Gow is a mountain, 1,770 metres (5,800 ft) high, on the east side of Rennick Glacier in the Bowers Mountains of Victoria Land, Antarctica. It marks the west end of the rugged heights between the mouths of Carryer Glacier and Sledgers Glacier where these two tributaries enter the nearby Rennick Glacier. This topographical feature was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–62, and was named by the Advisory Committee on Antarctic Names for Anthony J. Gow, a veteran Antarctic glaciologist who conducted his scientific research at the Byrd Station, South Pole Station, and McMurdo Station during nearly every Summer season ranging from 1959 to 1969. The mountain lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Carryer Glacier is a heavily crevassed tributary glacier, 12 nautical miles (22 km) long, which drains westward from the central part of the Bowers Mountains and enters Rennick Glacier between Mount Soza and Mount Gow, Victoria Land, Antarctica. The glacier was named by the northern party of New Zealand Geological Survey Antarctic Expedition, 1963–64, for S.J. Carryer, former geologist with this party. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Everett Range is a rugged, mainly ice-covered mountain range nearly 60 miles (97 km) long between Greenwell Glacier and Ebbe Glacier in northwest Victoria Land, Antarctica. Mountains of the range include Mount Regina. These mountains lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
The Greenwell Glacier is a major tributary glacier, 45 nautical miles long, draining northwest between the Mirabito Range and the Everett Range to enter Lillie Glacier below Mount Works, in northwest Victoria Land, Antarctica. This geographical feature was first mapped by the United States Geological Survey from surveys and from U.S. Navy aerial photography, 1960–63, and was so named by the Advisory Committee on Antarctic Names for Commander Martin D. Greenwell, U.S. Navy, Commander of Antarctic Squadron Six (VX-6), 1961–62. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
The Usarp Mountains is a major Antarctic mountain range, lying westward of the Rennick Glacier and trending N-S for about 190 kilometres (118 mi). The feature is bounded to the north by Pryor Glacier and the Wilson Hills. Its important constituent parts include Welcome Mountain, Mount Van der Hoeven, Mount Weihaupt, Mount Stuart, Mount Lorius, Smith Bench, Mount Roberts, Pomerantz Tableland, Daniels Range, Emlen Peaks, Helliwell Hills and Morozumi Range.
Ian Peak is a peak in the Bowers Mountains of Antarctica, 3 miles (5 km) northwest of Mount Stirling where the feature overlooks the heads of Leap Year Glacier and Champness Glacier. It was named by the New Zealand Geological Survey Antarctic Expedition, 1967–68, for Ian Smith of the Victoria University of Wellington, a geologist in Antarctica that season. The mountain lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Irwin Glacier is a steep tributary glacier in the Bowers Mountains of Antarctica, draining northeast from Edlin Névé and at the terminus coalescing with Montigny Glacier, with which it enters the larger Graveson Glacier. The glacier was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Carlisle S. Irwin, a former glaciologist who participated in the study of Meserve Glacier in 1966–67. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
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.
Astakhov Glacier is the glacier next south of Chugunov Glacier in the Explorers Range, Bowers Mountains. It flows northeast from Mount Hager and enters Ob' Bay just west of Platypus Ridge, the glacier is situated in Victoria Land, Antarctica. It was mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1960–65, and named by the Advisory Committee on Antarctic Names for Petr Astakhov, Soviet exchange scientist at the U.S. South Pole Station in 1967. The glacier lies on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Alamein Range is a mountain range lying west of Canham Glacier, in the Freyberg Mountains of Antarctica. Named in association with Lord Bernard Freyberg and the Second New Zealand Expeditionary Force by the Northern Party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963-64. The mountain range is situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Alt Glacier is a glacier in Antarctica. It is 4 nautical miles (7 km) long, flowing west-southwest from the Explorers Range of the Bowers Mountains to enter Rennick Glacier just north of Mount Soza. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Jean Alt, a French observer and weather central meteorologist at Little America V, winter party 1958. The glacier is situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Mount Bernstein is a prominent mountain, 2,420 m, which forms a part of the northern wall of Linder Glacier in the Lanterman Range, Bowers Mountains, a major mountain range situated in Victoria Land, Antarctica. The topographical feature was first mapped by the United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960-64. Named by Advisory Committee on Antarctic Names (US-ACAN) for the late Captain Fred J. Bernstein, Asst. Chief of Staff for Operations and Plans, U.S. Navy Support Force, Antarctica, 1967 and 1968. The mountain lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Bowers Peak is a peak, 2,140 metres (7,020 ft) high, forming a part of the divide between Hunter Glacier and Hoshko Glacier in the Lanterman Range, Bowers Mountains, a major mountain range situated in Victoria Land, Antarctica. The topographical feature was so named by the northern party of the New Zealand Geological Survey Antarctic Expedition, 1963–64, for Lieutenant John M. Bowers, Jr., of U.S. Navy Squadron VX-6, who flew support flights for this New Zealand field party. The peak lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Mount Janus is a bifurcated peak rising to 2,420 metres (7,940 ft) at the north side of the head of Montigny Glacier in the Bowers Mountains of Antarctica. It was named by the New Zealand Antarctic Place-Names Committee on the proposal of geologist R.A. Cooper, leader of a New Zealand Antarctic Research Programme geological party to the area, 1981–82, after Janus, the deity of portals in Roman mythology, symbolized as having two faces. The topographical feature lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Mount Draeger is a mountain, 1,690 metres (5,540 ft) high, in the northwest part of the Posey Range, Bowers Mountains, Victoria Land, Antarctica. The mountain overlooks from the east the junction of Smithson Glacier with the Graveson Glacier. The topographical feature was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–62, and was named by the Advisory Committee on Antarctic Names for chief radioman Ernest J. Draeger, U.S. Navy, a member of the winter party at McMurdo Station, Hut Point Peninsula, Ross Island, in 1967. The mountain lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Edlin Névé is a névé at the south side of Mount Sturm in the Bowers Mountains of Victoria Land, Antarctica. Several glaciers, including the Carryer, Irwin, McLin and Graveson, are nourished by this névé. it was named by the New Zealand Geological Survey Antarctic Expedition, 1967–68, for G. Edlin, who served as postmaster at Scott Base and assisted in the field during this expedition. This glaciological feature lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Mount Freed is a mountain, 2,120 metres (6,960 ft) high, that surmounts the divide between Champness Glacier and McCann Glacier, in the southern part of the Bowers Mountains of Victoria Land, Antarctica. The topographical feature was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–62, and was named by the Advisory Committee on Antarctic Names for Commander M.G. Freed, legal officer on the staff of the Commander, U.S. Naval Support Force, Antarctica, 1966–68. The mountain lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Graveson Glacier is a broad north-flowing tributary to the Lillie Glacier, draining that portion of the Bowers Mountains between the Posey Range and the southern part of Explorers Range, Victoria Land, Antarctica. The geographical feature is fed by several lesser tributaries and enters Lillie Glacier via Flensing Icefall. The glacier was so named by the northern party of the New Zealand Geological Survey Antarctic Expedition, 1963–64, for F. Graveson, a mining engineer who wintered at Scott Base in 1963 and was field assistant on this expedition. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Helix Pass is a small north–south pass 4 nautical miles (7 km) east-northeast of Mount Jamroga in the central Bowers Mountains of Victoria Land, Antarctica. The pass lies between two unnamed peaks and permits passage from the area at the head of Carryer Glacier to areas in the southern part of the Bowers Mountains. It was so named by the New Zealand Geological Survey Antarctic Expedition, 1967–68, because ascent of the pass required an all night trip with much zigzagging and climbing; thus named after the genus of land snail, Helix. This feature lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Hunter Glacier is a tributary glacier, 7 nautical miles (13 km) long, draining westward from the central Lanterman Range in the Bowers Mountains of Victoria Land, Antarctica and entering Rennick Glacier at Mount Lugering. It was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–62, and was so named by the Advisory Committee on Antarctic Names for Lieutenant Commander William G. Hunter, executive and operations officer with the McMurdo Station winter party in 1964. This glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Hoshko Glacier is a cirque-type glacier in the Lanterman Range of the Bowers Mountains in Victoria Land, Antarctica, draining southwest from between Bowers Peak and Mount Edixon into the lower part of Canham Glacier. This glacier was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Lieutenant John Hoshko, Jr., U.S. Navy Reserve, a public affairs officer on the staff of the Commander, U.S. Navy Support Force, Antarctica, 1966–68. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
The United States Geological Survey is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization has four major science disciplines, concerning biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility.
The Geographic Names Information System (GNIS) is a database that contains name and locative information about more than two million physical and cultural features located throughout the United States of America and its territories. It is a type of gazetteer. GNIS was developed by the United States Geological Survey in cooperation with the United States Board on Geographic Names (BGN) to promote the standardization of feature names.
This Victoria Land location article is a stub. You can help Wikipedia by expanding it. |