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Stillwell Hills is a group of largely snow-free rocky hills composed of banded gneisses and including Kemp Peak and Lealand Bluff, extending along the southwest side of William Scoresby Bay. This area was explored by Discovery Investigations personnel on the RSS William Scoresby in February 1936, and by the Lars Christensen Expedition, 1936–37, the latter group taking air photos used to map these hills for the first time. Geologic investigation of the area was made by Australian National Antarctic Research Expeditions (ANARE) in 1961. Named by ANCA for Dr. Frank Leslie Stillwell, geologist with Australasian Antarctic Expedition (AAE), 1911–14, who derived a theory of metamorphic differentiation from banded gneisses of the same type on George V Coast.

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  • Die Stillwell Hills sind eine Gruppe felsiger Hügel aus gebänderten Gneisen im ostantarktischen Kempland. Sie ragen am Südwestufer der William Scoresby Bay auf. Zu ihnen gehören der Kemp Peak und das Lealand Bluff. Wissenschaftler der britischen Discovery Investigations erkundeten sie im Februar 1936. Luftaufnahmen der Lars-Christensen-Expedition 1936/37 dienten ihrer Kartierung. Geologen der Australian National Antarctic Research Expeditions untersuchten sie im Jahr 1961. Das Antarctic Names Committee of Australia benannte sie nach dem australischen Geologen Frank Leslie Stillwell (1888–1963), Teilnehmer an der Australasiatischen Antarktisexpedition (1911–1914) des australischen Polarforschers Douglas Mawson. Stillwell hatte dabei eine Theorie der metamorphen Differenzierung gebänderter Gneise anhand entsprechender Funde an der Georg-V.-Küste entwickelt. (de)
  • Stillwell Hills is a group of largely snow-free rocky hills composed of banded gneisses and including Kemp Peak and Lealand Bluff, extending along the southwest side of William Scoresby Bay. This area was explored by Discovery Investigations personnel on the RSS William Scoresby in February 1936, and by the Lars Christensen Expedition, 1936–37, the latter group taking air photos used to map these hills for the first time. Geologic investigation of the area was made by Australian National Antarctic Research Expeditions (ANARE) in 1961. Named by ANCA for Dr. Frank Leslie Stillwell, geologist with Australasian Antarctic Expedition (AAE), 1911–14, who derived a theory of metamorphic differentiation from banded gneisses of the same type on George V Coast. (en)
  • Stillwell Hills – oaza antarktyczna na Ziemi Kempa na Antarktydzie. (pl)
  • Stillwellbergen (engelska: Stillwell Hills) är en antarktiska oas i östra Antarktis. (sv)
  • 史迪威山是南極洲的山峰,位於肯普地,處於威廉斯科斯比灣西南面,涵蓋肯普峰和利蘭海崖,以澳大利亞的地質學家命名,現時由南極條約體系管理。 (zh)
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  • Stillwell Hills is a group of largely snow-free rocky hills composed of banded gneisses and including Kemp Peak and Lealand Bluff, extending along the southwest side of William Scoresby Bay. This area was explored by Discovery Investigations personnel on the RSS William Scoresby in February 1936, and by the Lars Christensen Expedition, 1936–37, the latter group taking air photos used to map these hills for the first time. Geologic investigation of the area was made by Australian National Antarctic Research Expeditions (ANARE) in 1961. Named by ANCA for Dr. Frank Leslie Stillwell, geologist with Australasian Antarctic Expedition (AAE), 1911–14, who derived a theory of metamorphic differentiation from banded gneisses of the same type on George V Coast. (en)
  • Stillwell Hills – oaza antarktyczna na Ziemi Kempa na Antarktydzie. (pl)
  • Stillwellbergen (engelska: Stillwell Hills) är en antarktiska oas i östra Antarktis. (sv)
  • 史迪威山是南極洲的山峰,位於肯普地,處於威廉斯科斯比灣西南面,涵蓋肯普峰和利蘭海崖,以澳大利亞的地質學家命名,現時由南極條約體系管理。 (zh)
  • Die Stillwell Hills sind eine Gruppe felsiger Hügel aus gebänderten Gneisen im ostantarktischen Kempland. Sie ragen am Südwestufer der William Scoresby Bay auf. Zu ihnen gehören der Kemp Peak und das Lealand Bluff. (de)
rdfs:label
  • Stillwell Hills (de)
  • Stillwell Hills (pl)
  • Stillwell Hills (en)
  • Stillwellbergen (sv)
  • 史迪威山 (zh)
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