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http://dbpedia.org/ontology/abstract 瑟克塞申崖(英語:Succession Cliffs)是南極洲的懸崖,位於亞歷山大一世島東岸,全長2.8公里,最終在冥王星冰川入口以南注入喬治六世海峽,在1935年11月23日由美國探險家發現。 , Succession Cliffs (71°11′S 68°16′W / 71.Succession Cliffs (71°11′S 68°16′W / 71.183°S 68.267°W) is a line of steep cliffs 1.5 nautical miles (2.8 km) extending along the east coast of Alexander Island, Antarctica, facing east towards George VI Sound immediately south of the mouth of Pluto Glacier. The cliffs were probably first sighted by Lincoln Ellsworth who photographed segments of the coast in this vicinity on November 23, 1935. First roughly surveyed from the ground in 1936 by the British Graham Land Expedition and resurveyed in 1948 by the Falkland Islands Dependencies Survey. So named by the FIDS because a geologic succession, or depositional sequence, is revealed by the accessible rock exposures of the cliffs.e accessible rock exposures of the cliffs. , Die Succession Cliffs (von englisch succesDie Succession Cliffs (von englisch succession ‚Abfolge, Reihenfolge‘) sind eine Reihe steiler Kliffs von 2,5 km Länge an der Ostküste der westantarktischen Alexander-I.-Insel. Sie ragen unmittelbar südlich der Mündung des Pluto-Gletschers in den George-VI-Sund auf. Wahrscheinlich sichtete sie erstmals der US-amerikanische Polarforscher Lincoln Ellsworth bei seinem Transantarktisflug am 23. November 1935. Ellsworth fertigte Luftaufnahmen von der Küstenlinie in der Umgebung der Kliffs an. Teilnehmer der British Graham Land Expedition (1934–1937) unter der Leitung des australischen Polarforschers John Rymill nahmen 1936 eine grobe Vermessung vor. Der Falkland Islands Dependencies Survey (FIDS) verfeinerte diese im Jahr 1948. Der FIDS benannte sie nach der Abfolge der mineralischen Paragenesen im Gestein der Kliffs.lischen Paragenesen im Gestein der Kliffs.
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rdfs:comment 瑟克塞申崖(英語:Succession Cliffs)是南極洲的懸崖,位於亞歷山大一世島東岸,全長2.8公里,最終在冥王星冰川入口以南注入喬治六世海峽,在1935年11月23日由美國探險家發現。 , Succession Cliffs (71°11′S 68°16′W / 71.Succession Cliffs (71°11′S 68°16′W / 71.183°S 68.267°W) is a line of steep cliffs 1.5 nautical miles (2.8 km) extending along the east coast of Alexander Island, Antarctica, facing east towards George VI Sound immediately south of the mouth of Pluto Glacier. The cliffs were probably first sighted by Lincoln Ellsworth who photographed segments of the coast in this vicinity on November 23, 1935. First roughly surveyed from the ground in 1936 by the British Graham Land Expedition and resurveyed in 1948 by the Falkland Islands Dependencies Survey. So named by the FIDS because a geologic succession, or depositional sequence, is revealed by the accessible rock exposures of the cliffs.e accessible rock exposures of the cliffs. , Die Succession Cliffs (von englisch succesDie Succession Cliffs (von englisch succession ‚Abfolge, Reihenfolge‘) sind eine Reihe steiler Kliffs von 2,5 km Länge an der Ostküste der westantarktischen Alexander-I.-Insel. Sie ragen unmittelbar südlich der Mündung des Pluto-Gletschers in den George-VI-Sund auf.luto-Gletschers in den George-VI-Sund auf.
rdfs:label Succession Cliffs , 瑟克塞申崖
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