Hoskins Peak

Last updated

Hoskins Peak ( 67°46′S67°36′W / 67.767°S 67.600°W / -67.767; -67.600 Coordinates: 67°46′S67°36′W / 67.767°S 67.600°W / -67.767; -67.600 ) is a peak 3 nautical miles (6 km) west of Contact Peak in southern Pourquoi Pas Island, Graham Land, Antarctica. It was mapped by the Falkland Islands Dependencies Survey (FIDS) from surveys, 1956–59, and named by the UK Antarctic Place-Names Committee for Arthur K. Hoskins, a FIDS geologist at Stonington Island in 1958 and Horseshoe Island in 1959. [1]

Geographic coordinate system Coordinate system

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.

Contact Peak is a prominent rock peak, 1,005 metres (3,300 ft) high, which is the southeasternmost peak on Pourquoi Pas Island, off the west coast of Graham Land. It was first sighted and roughly charted in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot. It was surveyed in 1936 by the British Graham Land Expedition and in 1948 by the Falkland Islands Dependencies Survey (FIDS). It was so named by FIDS because the peak marks the granite-volcanic contact in the cliffs which is visible at a considerable distance.

Pourquoi Pas Island

Pourquoi Pas Island is a mountainous island, 27 km (17 mi) long and from 8 to 18 km wide, lying between Bigourdan Fjord and Bourgeois Fjord off the west coast of Graham Land. It was discovered by the French Antarctic Expedition under Charcot, 1908-10. The island was charted more accurately by the British Graham Land Expedition (BGLE) under John Rymill, 1934–37, who named it for Charcot's expedition ship, the Pourquoi-Pas.

Related Research Articles

Cape Brooks is a cape marked by steep, conspicuous walls which rise to 465 metres (1,530 ft), forming the south side of the entrance to New Bedford Inlet, on the east coast of Palmer Land. It was discovered and photographed from the air in December 1940 by members of the US Antarctic Service, and again photographed from the air in 1947 by members of the Ronne Antarctic Research Expedition, who in conjunction with the Falkland Islands Dependencies Survey (FIDS) also charted it from the ground. Cape Brooks was named by the FIDS for Charles E.P. Brooks, an English meteorologist on the staff of the Meteorological Office, from 1907 to 1949.

Aagaard Glacier glacier in Antarctica

Aagaard Glacier, also known as Glaciar Alderete, is an 8-mile (13 km) long Antarctic glacier which lies close to the east of Gould Glacier and flows in a southerly direction into Mill Inlet, on the east coast of Graham Land. It was charted by the Falkland Islands Dependencies Survey (FIDS) and photographed from the air by the Ronne Antarctic Research Expedition during December 1947; it was named by the FIDS for Bjarne Aagaard, a Norwegian authority on Antarctic whaling and exploration.

Kichenside Glacier glacier in Antarctica

Kichenside Glacier is a glacier, 15 nautical miles (28 km) long and 3 to 5 nautical miles wide, flowing northeast into the southern part of the Hannan Ice Shelf on the coast of Enderby Land, Antarctica. It was charted from air photos taken from an Australian National Antarctic Research Expeditions aircraft in 1956, and was named by the Antarctic Names Committee of Australia for Squadron Leader James C. Kichenside, RAAF, officer commanding the Antarctic Flight at Mawson Station in 1960.

Attlee Glacier glacier in Antarctica

Attlee Glacier is a glacier 8 miles (13 km) long, which flows east-southeast from the plateau escarpment on the east side of Graham Land to the head of Cabinet Inlet to the north of Bevin Glacier. During December 1947, the glacier was charted from the ground by the Falkland Islands Dependencies Survey (FIDS) and photographed from the air by the Ronne Antarctic Research Expedition. It was named by the FIDS for Rt. Hon. Clement Attlee, M.P., British Secretary of State for Dominion Affairs, member of the War Cabinet, and later Prime Minister of the United Kingdom.

Harmer Glacier glacier in Antarctica

Harmer Glacier is a glacier 3 nautical miles (6 km) long, flowing southwest from Starbuck Peak to the sea close north of Ranvik, on the south coast of South Georgia. It was surveyed by the South Georgia Survey in the period 1951–57, and named by the UK Antarctic Place-Names Committee for Sir Sidney F. Harmer.

Orel Ice Fringe is a strip of coastal ice bordering the south side of Errera Channel between Beneden Head and Porro Bluff, on the west coast of Graham Land. Mapped by the Falkland Islands Dependencies Survey (FIDS) from photos taken by Hunting Aerosurveys Ltd. in 1956-57. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1960 for Eduard von Orel (1877–1941), Austrian surveyor who in 1905 designed the first stereoautograph for plotting maps directly from horizontal photographs.

Widdowson Glacier

Widdowson Glacier is a glacier situated between Drummond and McCance Glaciers and flowing into Darbel Bay south of Sokol Point, on the west coast of Graham Land.

Swift Glacier glacier in Antarctica

Swift Glacier is a steep glacier about 2 nautical miles (3.7 km) long, close west of Jefford Point, James Ross Island. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) following Falkland Islands Dependencies Survey (FIDS) surveys, 1958-61. The name is descriptive, this being one of the most active glaciers on the island.

Swithinbank Glacier

Swithinbank Glacier is a glacier on the west side of Hemimont Plateau flowing north to the southeast corner of Square Bay, in Graham Land. Mapped by Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1946-59. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Charles Swithinbank, British glaciologist, a participant in several British, New Zealand and American expeditions to Antarctica, 1949-62.

Perutz Glacier glacier in Antarctica

Perutz Glacier is a glacier, 10 nautical miles (18 km) long and 2 nautical miles (3.7 km) wide, which flows west-northwest from Hemimont Plateau into Bourgeois Fjord, close east of Thomson Head, on the west coast of Graham Land, Antarctica. The mouth of the glacier was first surveyed in 1936 by the British Graham Land Expedition (BGLE) under Rymill. The entire glacier was surveyed in 1946-47 and 1948-49 by the Falkland Islands Dependencies Survey (FIDS), and named by them for Max F. Perutz of the Cavendish Laboratory, Cambridge, who has made important studies on the mechanism of glacier flow.

Glen Peak is a peak on the north end of Liard Island in Hanusse Bay, Antarctica. It was mapped from air photos obtained by the Ronne Antarctic Research Expedition (1947–48) and the Falkland Islands and Dependencies Aerial Survey Expedition (1956–57). It was named by the UK Antarctic Place-Names Committee for John W. Glen, a British physicist who has made laboratory investigations on the flow of single and polycrystalline ice.

Mimas Peak is a sharp conspicuous peak, rising to about 1,000 metres (3,300 ft) west of the head of Saturn Glacier and 9 nautical miles (17 km) west of the Dione Nunataks in the southeast part of Alexander Island, Antarctica. It was first seen and photographed from the air by Lincoln Ellsworth on November 23, 1935, and mapped from these photos by W.L.G. Joerg. The peak was sighted from a distance in 1949 by the Falkland Islands Dependencies Survey (FIDS) and roughly positioned. It was named by the UK Antarctic Place-Names Committee for its association with nearby Saturn Glacier, Mimas being one of the satellites of the planet Saturn. The peak and surrounding area were first mapped in detail from air photos taken by the Ronne Antarctic Research Expedition 1947–48, by D. Searle of the FIDS in 1960.

Harris Peak is a peak, 1,005 metres (3,300 ft) high, surmounting the base of Reclus Peninsula on the west coast of Graham Land, Antarctica. It was mapped by the Falkland Islands Dependencies Survey (FIDS) from photos taken by Hunting Aerosurveys Ltd in 1956–57, and was named by the UK Antarctic Place-Names Committee in 1960 for Leslie Harris, a FIDS carpenter and general assistant at the Danco Island station in 1956, who participated in the reconnaissance journeys from that station and from the nearby Portal Point hut.

Hunt Peak is a triangular rock peak, 610 metres (2,000 ft) high, marking the north side of the entrance to Stonehouse Bay on the east coast of Adelaide Island, Antarctica. It was discovered and first roughly surveyed in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot. It was resurveyed in 1948 by the Falkland Islands Dependencies Survey (FIDS), who named the point marked by this peak for Sergeant Kenneth D. Hunt, a mechanic for the expedition's Noorduyn Norseman airplane in 1950. Further survey in 1957–58 by the FIDS showed no definable point in the vicinity and the name was transferred to the peak.

Skinner Peak is a mainly snow-covered peak, over 2,600 m, on the spur that descends northeast from Mount Schopf in Ohio Range, Horlick Mountains. Named by Advisory Committee on Antarctic Names (US-ACAN) for Courtney J. Skinner, geological assistant and camp manager with the Ohio State University expedition to the Horlick Mountains in 1961-62. Skinner visited Antarctica with United States Antarctic Research Program (USARP) every summer season from 1961-62 to 1966-67.

Kalafut Nunatak is a nunatak which marks the southeast end of the Haines Mountains, in the Ford Ranges of Marie Byrd Land, Antarctica. It was mapped by the United States Antarctic Service (1939–41) and by the United States Geological Survey from surveys and U.S. Navy air photos (1959–65). It was named by the Advisory Committee on Antarctic Names for John Kalafut, a United States Antarctic Research Program glaciologist at Byrd Station in the 1966–67 and 1968–69 seasons.

Thomson Head headland

Thomson Head is a steep, rocky headland rising to 915 m at the east side of Bourgeois Fjord, between Perutz and Bader Glaciers, forming the north extremity of German Peninsula on Fallières Coast on the west side of Graham Land, Antarctica. First surveyed in 1936 by the British Graham Land Expedition (BGLE) under Rymill. Resurveyed in 1948-49 by the Falkland Islands Dependencies Survey (FIDS) and named for William H. Thomson, FIDS air pilot at Stonington Island in 1947.

Vallot Glacier is a glacier flowing northwest to Laubeuf Fjord close south of Lewis Peaks, on Arrowsmith Peninsula in Graham Land. It was mapped by the Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1948–59, and was named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for Joseph Vallot, a French naturalist and glaciologist who first measured the surface velocity of a glacier over a long period, in Switzerland, 1891-99.

Larssen Peak is a peak, 1,550 metres (5,100 ft) high, between the Three Brothers and Marikoppa in the Allardyce Range of South Georgia. It was surveyed by the South Georgia Survey in the period 1951–57, and named by the UK Antarctic Place-Names Committee for Harald Larssen, manager at the Compañía Argentina de Pesca station, Grytviken, 1951–54.

References

PD-icon.svg This article incorporates  public domain material from the United States Geological Survey document "Hoskins Peak" (content from the Geographic Names Information System ).

United States Geological Survey Scientific agency of the United States government

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.

Geographic Names Information System geographical database

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.