Simpson Glacier (71°17′S 168°38′E / 71.283°S 168.633°E) is a glacier, 6 miles (10 km) long, in the Admiralty Mountains. It flows northward to the coast between Nelson Cliff and Mount Cherry-Garrard where it forms the Simpson Glacier Tongue. The latter feature was named by the British Antarctic Expedition, 1910–13, after Sir George Simpson, meteorologist of the expedition. The glacier described was mapped by United States Geological Survey (USGS), 1960–63,a and was so named by Advisory Committee on Antarctic Names (US-ACAN) because (with Fendley Glacier to the east) it nourishes the Simpson Glacier Tongue.
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| - Simpson-Gletscher (de)
- Ghiacciaio Simpson (it)
- Simpson Glacier (en)
- Simpson Glacier (sv)
- 辛普森冰川 (zh)
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| - Il ghiacciaio Simpson è un ghiacciaio lungo circa 10 km situato sulla costa di Pennell, nella regione nord-occidentale della Dipendenza di Ross, in Antartide. In particolare, il ghiacciaio, il cui punto più alto si trova a circa 1200 m s.l.m., ha origine nella parte settentrionale dei monti dell'Ammiragliato, in particolare da una posizione subito a ovest del , e da qui fluisce in direzione nord, scorrendo lungo il versante occidentale del suddetto monte, fino ad entrare nell'estremità occidentale della baia di Robertson, poco a est della , unendosi all'estremità orientale del ghiacciaio Fendley e alimentando la . (it)
- Simpson Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Nya Zeeland gör anspråk på området. Simpson Glacier ligger 622 meter över havet. Terrängen runt Simpson Glacier är varierad. Den högsta punkten i närheten är 1 088 meter över havet, 1,8 kilometer söder om Simpson Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. (sv)
- 辛普森冰川是南極洲的冰川,位於維多利亞地的彭內爾海岸,全長10公里,終點在納爾遜崖和徹里加勒德山之間,由英國探險隊的氣象學家命名。 (zh)
- Der Simpson-Gletscher ist ein 10 km langer Gletscher in den Admiralitätsbergen im Norden des ostantarktischen Viktorialands. Er fließt in nördlicher Richtung zwischen dem Nelson-Kliff und dem Mount Cherry-Garrard und läuft in Form einer kleinen Gletscherzunge (71° 15′ S, 168° 45′ O), die auch das Ende des Fendley-Gletschers markiert, an der Pennell-Küste in die Somow-See aus. (de)
- Simpson Glacier (71°17′S 168°38′E / 71.283°S 168.633°E) is a glacier, 6 miles (10 km) long, in the Admiralty Mountains. It flows northward to the coast between Nelson Cliff and Mount Cherry-Garrard where it forms the Simpson Glacier Tongue. The latter feature was named by the British Antarctic Expedition, 1910–13, after Sir George Simpson, meteorologist of the expedition. The glacier described was mapped by United States Geological Survey (USGS), 1960–63,a and was so named by Advisory Committee on Antarctic Names (US-ACAN) because (with Fendley Glacier to the east) it nourishes the Simpson Glacier Tongue. (en)
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| - Der Simpson-Gletscher ist ein 10 km langer Gletscher in den Admiralitätsbergen im Norden des ostantarktischen Viktorialands. Er fließt in nördlicher Richtung zwischen dem Nelson-Kliff und dem Mount Cherry-Garrard und läuft in Form einer kleinen Gletscherzunge (71° 15′ S, 168° 45′ O), die auch das Ende des Fendley-Gletschers markiert, an der Pennell-Küste in die Somow-See aus. Die Gletscherzunge wurde von Teilnehmern der Terra-Nova-Expedition (1910–1913) nach George Clarke Simpson (1878–1965) benannt, dem Meteorologen der Expedition. Der Gletscher selbst wurde vom United States Geological Survey zwischen 1960 und 1963 kartiert. Das Advisory Committee on Antarctic Names übernahm 1970 die Benennung der Gletscherzunge auch für den Gletscher. (de)
- Simpson Glacier (71°17′S 168°38′E / 71.283°S 168.633°E) is a glacier, 6 miles (10 km) long, in the Admiralty Mountains. It flows northward to the coast between Nelson Cliff and Mount Cherry-Garrard where it forms the Simpson Glacier Tongue. The latter feature was named by the British Antarctic Expedition, 1910–13, after Sir George Simpson, meteorologist of the expedition. The glacier described was mapped by United States Geological Survey (USGS), 1960–63,a and was so named by Advisory Committee on Antarctic Names (US-ACAN) because (with Fendley Glacier to the east) it nourishes the Simpson Glacier Tongue. This article incorporates public domain material from "Simpson Glacier". Geographic Names Information System. United States Geological Survey.
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* e (en)
- Il ghiacciaio Simpson è un ghiacciaio lungo circa 10 km situato sulla costa di Pennell, nella regione nord-occidentale della Dipendenza di Ross, in Antartide. In particolare, il ghiacciaio, il cui punto più alto si trova a circa 1200 m s.l.m., ha origine nella parte settentrionale dei monti dell'Ammiragliato, in particolare da una posizione subito a ovest del , e da qui fluisce in direzione nord, scorrendo lungo il versante occidentale del suddetto monte, fino ad entrare nell'estremità occidentale della baia di Robertson, poco a est della , unendosi all'estremità orientale del ghiacciaio Fendley e alimentando la . (it)
- Simpson Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Nya Zeeland gör anspråk på området. Simpson Glacier ligger 622 meter över havet. Terrängen runt Simpson Glacier är varierad. Den högsta punkten i närheten är 1 088 meter över havet, 1,8 kilometer söder om Simpson Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. (sv)
- 辛普森冰川是南極洲的冰川,位於維多利亞地的彭內爾海岸,全長10公里,終點在納爾遜崖和徹里加勒德山之間,由英國探險隊的氣象學家命名。 (zh)
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| - POINT(168.63333129883 -71.283332824707)
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