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Magnetite Bluff (83°22′S 51°15′W / 83.367°S 51.250°W) is a bluff 2 nautical miles (4 km) northeast of Mount Stephens on the west side of Saratoga Table, in the Forrestal Range of Antarctica. It was named by the Advisory Committee on Antarctic Names in 1979, at the suggestion of and following United States Geological Survey geological work in the area, from the extensive occurrences of magnetite in the gabbro of this area, which cause large magnetic anomalies over the Forrestal Range.

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  • Das Magnetite Bluff ist ein 1710 m hohes Felsenkliff im westantarktischen Queen Elizabeth Land. In der Forrestal Range der Pensacola Mountains ragt es 3 km nordöstlich des Mount Stephens an der Westseite des Saratoga Table auf. Das Advisory Committee on Antarctic Names benannte es 1979 auf Vorschlag des US-amerikanischen Geologen Arthur B. Ford. Namensgebend ist das große Vorkommen an Magnetit im Gabbrogestein dieser Region, das große magnetische Anomalien in der Forrestal Range verursacht. (de)
  • Magnetite Bluff (83°22′S 51°15′W / 83.367°S 51.250°W) is a bluff 2 nautical miles (4 km) northeast of Mount Stephens on the west side of Saratoga Table, in the Forrestal Range of Antarctica. It was named by the Advisory Committee on Antarctic Names in 1979, at the suggestion of and following United States Geological Survey geological work in the area, from the extensive occurrences of magnetite in the gabbro of this area, which cause large magnetic anomalies over the Forrestal Range. (en)
  • La Magnetite Bluff (in lingua inglese: Falesia della magnetite) è una falesia antartica situata 4 km a nordest del Monte Stephens, nel fianco occidentale della Saratoga Table, nel Forrestal Range dei Monti Pensacola, in Antartide. La denominazione è stata assegnata dall'Advisory Committee on Antarctic Names (US-ACAN) su proposta del geologo Arthur B. Ford, in seguito alle indagini geologiche svolte in quest'area dall'United States Geological Survey (USGS), in riferimento alla magnetite presente in notevole quantità nel gabbro di questa zona, che causa importanti anomalie magnetiche nel Forrestal Range. (it)
  • 馬格尼泰特海崖(英語:Magnetite Bluff)是南極洲的海崖,位於伊莉莎白女王地,處於斯蒂芬斯山東北面4公里,屬於福里斯特爾山脈的一部分,現時由南極條約體系管理。 (zh)
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  • Das Magnetite Bluff ist ein 1710 m hohes Felsenkliff im westantarktischen Queen Elizabeth Land. In der Forrestal Range der Pensacola Mountains ragt es 3 km nordöstlich des Mount Stephens an der Westseite des Saratoga Table auf. Das Advisory Committee on Antarctic Names benannte es 1979 auf Vorschlag des US-amerikanischen Geologen Arthur B. Ford. Namensgebend ist das große Vorkommen an Magnetit im Gabbrogestein dieser Region, das große magnetische Anomalien in der Forrestal Range verursacht. (de)
  • Magnetite Bluff (83°22′S 51°15′W / 83.367°S 51.250°W) is a bluff 2 nautical miles (4 km) northeast of Mount Stephens on the west side of Saratoga Table, in the Forrestal Range of Antarctica. It was named by the Advisory Committee on Antarctic Names in 1979, at the suggestion of and following United States Geological Survey geological work in the area, from the extensive occurrences of magnetite in the gabbro of this area, which cause large magnetic anomalies over the Forrestal Range. (en)
  • 馬格尼泰特海崖(英語:Magnetite Bluff)是南極洲的海崖,位於伊莉莎白女王地,處於斯蒂芬斯山東北面4公里,屬於福里斯特爾山脈的一部分,現時由南極條約體系管理。 (zh)
  • La Magnetite Bluff (in lingua inglese: Falesia della magnetite) è una falesia antartica situata 4 km a nordest del Monte Stephens, nel fianco occidentale della Saratoga Table, nel Forrestal Range dei Monti Pensacola, in Antartide. (it)
rdfs:label
  • Magnetite Bluff (de)
  • Magnetite Bluff (it)
  • Magnetite Bluff (en)
  • 馬格尼泰特海崖 (zh)
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