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The Keystone Cliffs (71°35′S 68°13′W / 71.583°S 68.217°W) are a set of cliffs, 610 metres (2,000 ft) high, marking the east face of the sedimentary ridge between Mercury Glacier and Venus Glacier, on the east coast of Alexander Island, Antarctica. The coast in this vicinity was first seen from the air by Lincoln Ellsworth on November 23, 1935, and roughly mapped from photos obtained on that flight by W.L.G. Joerg. The cliffs were roughly surveyed in 1936 by the British Graham Land Expedition and resurveyed in 1948 by the Falkland Islands Dependencies Survey (FIDS). They were so named by the FIDS because the geologic structures revealed in these cliffs provided the key to the general tectonic structure of the area.

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  • Keystone-Kliffs (de)
  • Keystone Cliffs (en)
  • 基斯唐崖 (zh)
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  • Die Keystone-Kliffs sind 610 m hohe Kliffs an der Ostküste der westantarktischen Alexander-I.-Insel. Sie bilden die Ostflanke eines Gebirgskamms aus Sedimentgestein zwischen dem Merkur-Gletscher und dem Venus-Gletscher. Die Kliffs wurden 1936 bei der British Graham Land Expedition (1934–1937) und 1948 durch den Falkland Islands Dependencies Survey (FIDS) vermessen. Der FIDS benannte die Kliffs so, weil ihr Gestein (englisch stone) den sinnbildlichen Schlüssel (englisch key) zur allgemeinen tektonischen Struktur des Gebiets darstellt. (de)
  • The Keystone Cliffs (71°35′S 68°13′W / 71.583°S 68.217°W) are a set of cliffs, 610 metres (2,000 ft) high, marking the east face of the sedimentary ridge between Mercury Glacier and Venus Glacier, on the east coast of Alexander Island, Antarctica. The coast in this vicinity was first seen from the air by Lincoln Ellsworth on November 23, 1935, and roughly mapped from photos obtained on that flight by W.L.G. Joerg. The cliffs were roughly surveyed in 1936 by the British Graham Land Expedition and resurveyed in 1948 by the Falkland Islands Dependencies Survey (FIDS). They were so named by the FIDS because the geologic structures revealed in these cliffs provided the key to the general tectonic structure of the area. (en)
  • 基斯唐崖（英語：Keystone Cliffs）是南極洲的懸崖，位於亞歷山大一世島東岸，處於水星冰川和金星冰川之間，海拔高度610米，在1935年11月23日由美國的探險家發現。 (zh)
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  • -71.58333333333333 -68.21666666666667
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  • Die Keystone-Kliffs sind 610 m hohe Kliffs an der Ostküste der westantarktischen Alexander-I.-Insel. Sie bilden die Ostflanke eines Gebirgskamms aus Sedimentgestein zwischen dem Merkur-Gletscher und dem Venus-Gletscher. Die Kliffs wurden 1936 bei der British Graham Land Expedition (1934–1937) und 1948 durch den Falkland Islands Dependencies Survey (FIDS) vermessen. Der FIDS benannte die Kliffs so, weil ihr Gestein (englisch stone) den sinnbildlichen Schlüssel (englisch key) zur allgemeinen tektonischen Struktur des Gebiets darstellt. (de)
  • The Keystone Cliffs (71°35′S 68°13′W / 71.583°S 68.217°W) are a set of cliffs, 610 metres (2,000 ft) high, marking the east face of the sedimentary ridge between Mercury Glacier and Venus Glacier, on the east coast of Alexander Island, Antarctica. The coast in this vicinity was first seen from the air by Lincoln Ellsworth on November 23, 1935, and roughly mapped from photos obtained on that flight by W.L.G. Joerg. The cliffs were roughly surveyed in 1936 by the British Graham Land Expedition and resurveyed in 1948 by the Falkland Islands Dependencies Survey (FIDS). They were so named by the FIDS because the geologic structures revealed in these cliffs provided the key to the general tectonic structure of the area. (en)
  • 基斯唐崖（英語：Keystone Cliffs）是南極洲的懸崖，位於亞歷山大一世島東岸，處於水星冰川和金星冰川之間，海拔高度610米，在1935年11月23日由美國的探險家發現。 (zh)
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  • POINT(-68.216667175293 -71.583335876465)
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