Skidmore Cliff (original) (raw)

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Skidmore Cliff (83°24′S 49°30′W / 83.400°S 49.500°W) is an irregular east-facing cliff, 4 nautical miles (7 km) long, located at the extremity of a spur trending eastward from Saratoga Table, in the Forrestal Range, Pensacola Mountains, Antarctica. It was mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photographs during 1956–66. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for , an ionospheric scientist at Ellsworth Station, during the winter of 1957.

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dbo:abstract Das Skidmore-Kliff ist ein unregelmäßig geformtes, nach Osten ausgerichtetes, 6 km langes und 1185 m hohes Felsenkliff im westantarktischen Queen Elizabeth Land. In der Forrestal Range der Pensacola Mountains ragt es am Ende eines sich vom Saratoga Table nach Osten erstreckenden Felssporns auf. Der United States Geological Survey kartierte es anhand eigener Vermessungen und Luftaufnahmen der United States Navy aus den Jahren von 1956 bis 1966. Das Advisory Committee on Antarctic Names benannte es 1968 nach Donald D. Skidmore, Ionosphärenphysiker auf der Ellsworth-Station im antarktischen Winter 1957. (de) Skidmore Cliff (83°24′S 49°30′W / 83.400°S 49.500°W) is an irregular east-facing cliff, 4 nautical miles (7 km) long, located at the extremity of a spur trending eastward from Saratoga Table, in the Forrestal Range, Pensacola Mountains, Antarctica. It was mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photographs during 1956–66. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for , an ionospheric scientist at Ellsworth Station, during the winter of 1957. (en) La Skidmore Cliff (in lingua inglese: Scogliera Skidmore) è una parete rocciosa irregolare, orientata verso est e lunga 7 km, situata all'estremità di uno sperone roccioso che si sviluppa in direzione est a partire dalla Saratoga Table del Forrestal Range, nei Monti Pensacola, in Antartide. La scogliera è stata mappata dall'United States Geological Survey (USGS) sulla base di rilevazioni e foto aeree scattate dalla U.S. Navy nel periodo 1956-66. La denominazione è stata assegnata dall'Advisory Committee on Antarctic Names (US-ACAN) in onore di Donald D. Skidmore, che ha condotto studi sulla ionosfera presso la Stazione Ellsworth nell'inverno del 1957. (it) 斯基德莫爾崖(英語:Skidmore Cliff)是南極洲的山崖,位於伊莉莎白女王地,屬於彭薩科拉山脈中福里斯特爾山脈的一部分,長7公里,美國地質調查局根據測量和該國海軍的空中照片繪入地圖,現時由南極條約體系管理。 (zh)
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rdfs:comment Skidmore Cliff (83°24′S 49°30′W / 83.400°S 49.500°W) is an irregular east-facing cliff, 4 nautical miles (7 km) long, located at the extremity of a spur trending eastward from Saratoga Table, in the Forrestal Range, Pensacola Mountains, Antarctica. It was mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photographs during 1956–66. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for , an ionospheric scientist at Ellsworth Station, during the winter of 1957. (en) 斯基德莫爾崖(英語:Skidmore Cliff)是南極洲的山崖,位於伊莉莎白女王地,屬於彭薩科拉山脈中福里斯特爾山脈的一部分,長7公里,美國地質調查局根據測量和該國海軍的空中照片繪入地圖,現時由南極條約體系管理。 (zh) Das Skidmore-Kliff ist ein unregelmäßig geformtes, nach Osten ausgerichtetes, 6 km langes und 1185 m hohes Felsenkliff im westantarktischen Queen Elizabeth Land. In der Forrestal Range der Pensacola Mountains ragt es am Ende eines sich vom Saratoga Table nach Osten erstreckenden Felssporns auf. (de) La Skidmore Cliff (in lingua inglese: Scogliera Skidmore) è una parete rocciosa irregolare, orientata verso est e lunga 7 km, situata all'estremità di uno sperone roccioso che si sviluppa in direzione est a partire dalla Saratoga Table del Forrestal Range, nei Monti Pensacola, in Antartide. La scogliera è stata mappata dall'United States Geological Survey (USGS) sulla base di rilevazioni e foto aeree scattate dalla U.S. Navy nel periodo 1956-66. (it)
rdfs:label Skidmore-Kliff (de) Skidmore Cliff (it) Skidmore Cliff (en) 斯基德莫爾崖 (zh)
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