The Mohn Basin (86°30′S 168°0′W / 86.500°S 168.000°W) is a major depression in the surface near the edge of the Antarctic polar plateau. It extends southward from the western limit of the Quarles Range for about 100 nautical miles (200 km) and includes the névé area adjacent to the heads of the Bowman, Devils, Amundsen and Scott glaciers, in the Queen Maud Mountains of Antarctica. The feature was encountered in December 1911 by the South Pole party of the Norwegian expedition under Roald Amundsen, and was named by the Advisory Committee on Antarctic Names for Norwegian meteorologist Henrik Mohn, the author of the meteorological report of this expedition.
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| - Mohn Basin (de)
- Mohn Basin (it)
- Mohn Basin (en)
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| - The Mohn Basin (86°30′S 168°0′W / 86.500°S 168.000°W) is a major depression in the surface near the edge of the Antarctic polar plateau. It extends southward from the western limit of the Quarles Range for about 100 nautical miles (200 km) and includes the névé area adjacent to the heads of the Bowman, Devils, Amundsen and Scott glaciers, in the Queen Maud Mountains of Antarctica. The feature was encountered in December 1911 by the South Pole party of the Norwegian expedition under Roald Amundsen, and was named by the Advisory Committee on Antarctic Names for Norwegian meteorologist Henrik Mohn, the author of the meteorological report of this expedition. (en)
- Das Mohn Basin ist eine große Senke am Rand des Polarplateaus in der antarktischen Ross Dependency. Sie erstreckt sich vom Westrand der Quarles Range südwärts über eine Strecke von 160 km und schließt das Firnfeldgebiet im Königin-Maud-Gebirge mit ein, das an die Kopfenden des Bowman-Gletschers, des Devils Glacier, des Amundsen- und des Scott-Gletschers grenzt. (de)
- Il Mohn Basin (in lingua inglese: Bacino Mohn) è una vasta depressione della superficie antartica, situata in prossimità del bordo dell'Altopiano Antartico. Si estende in direzione sud per 200 km a partire dall'estremità occidentale del Quarles Range e include il l'area del nevaio adiacente alla testa dei ghiacciai Bowman, , Amundsen e Scott, nei Monti della Regina Maud, in Antartide. Fu scoperto nel dicembre 1911 dal gruppo diretto verso il Polo Sud della spedizione antartica guidata dall'esploratore norvegese Roald Amundsen. (it)
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| - Das Mohn Basin ist eine große Senke am Rand des Polarplateaus in der antarktischen Ross Dependency. Sie erstreckt sich vom Westrand der Quarles Range südwärts über eine Strecke von 160 km und schließt das Firnfeldgebiet im Königin-Maud-Gebirge mit ein, das an die Kopfenden des Bowman-Gletschers, des Devils Glacier, des Amundsen- und des Scott-Gletschers grenzt. Der norwegische Polarforscher Roald Amundsen und vier Begleiter entdeckten die Senke im Zuge seiner erfolgreichen Südpolexpedition (1910–1912) im Dezember 1911. Das Advisory Committee on Antarctic Names benannte sie nach dem norwegischen Meteorologen Henrik Mohn (1835–1916), der die meteorologischen Berichte zu Amundsens Forschungsreise geschrieben hatte. (de)
- The Mohn Basin (86°30′S 168°0′W / 86.500°S 168.000°W) is a major depression in the surface near the edge of the Antarctic polar plateau. It extends southward from the western limit of the Quarles Range for about 100 nautical miles (200 km) and includes the névé area adjacent to the heads of the Bowman, Devils, Amundsen and Scott glaciers, in the Queen Maud Mountains of Antarctica. The feature was encountered in December 1911 by the South Pole party of the Norwegian expedition under Roald Amundsen, and was named by the Advisory Committee on Antarctic Names for Norwegian meteorologist Henrik Mohn, the author of the meteorological report of this expedition. (en)
- Il Mohn Basin (in lingua inglese: Bacino Mohn) è una vasta depressione della superficie antartica, situata in prossimità del bordo dell'Altopiano Antartico. Si estende in direzione sud per 200 km a partire dall'estremità occidentale del Quarles Range e include il l'area del nevaio adiacente alla testa dei ghiacciai Bowman, , Amundsen e Scott, nei Monti della Regina Maud, in Antartide. Fu scoperto nel dicembre 1911 dal gruppo diretto verso il Polo Sud della spedizione antartica guidata dall'esploratore norvegese Roald Amundsen. La denominazione fu assegnata dall'Advisory Committee on Antarctic Names (US-ACAN), in onore del meteorologo norvegese Henrik Mohn (1835-1916), autore del resoconto meteorologico della spedizione. (it)
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