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http://dbpedia.org/ontology/abstract Cassidy Glacier är en glaciär i Antarktis.Cassidy Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Nya Zeeland gör anspråk på området. Cassidy Glacier ligger 1 785 meter över havet. Terrängen runt Cassidy Glacier är kuperad åt sydost, men åt nordväst är den platt. Den högsta punkten i närheten är Marvin Nunatak, 2 090 meter över havet, 2,4 kilometer väster om Cassidy Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten.lkad. Det finns inga samhällen i närheten. , Il ghiacciaio Cassidy è un ghiacciaio lungIl ghiacciaio Cassidy è un ghiacciaio lungo circa 13 km situato nella regione centro-occidentale della Dipendenza di Ross, in Antartide. Il ghiacciaio, il cui punto più alto si trova a circa 2000 m s.l.m., si trova in particolare tra le montagne di Quartermain, a est, e il , a ovest, nell'entroterra della costa di Scott, dove fluisce verso nord-est fino a unire il proprio flusso, a cui nel frattempo si è unito quello di altri ghiacciai come il Fitzpatrick e il Fireman, a quello del ghiacciaio Taylor.l Fireman, a quello del ghiacciaio Taylor. , Der Cassidy-Gletscher ist ein rund 11 km lDer Cassidy-Gletscher ist ein rund 11 km langer langer und 3 km breiter Gletscher im ostantarktischen Viktorialand. Er fließt in nordöstlicher Richtung zwischen dem Depot-Nunatak und dem nordwestlichen Ende der Quartermain Mountains in den oberen Abschnitt des Taylor-Gletschers. Beschrieben wurde das Gebiet des Gletschers erstmals durch Teilnehmer der Discovery-Expedition (1901–1904) unter der Leitung des britischen Polarforschers Robert Falcon Scott. Das Advisory Committee on Antarctic Names benannte ihn im Jahr 1992 nach William A. Cassidy vom Department of Geology and Planetary Science der University of Pittsburgh, der zwischen 1976 und 1990 in dreizehn Kampagnen des United States Antarctic Program Expeditionsmannschaften zur Sammlung antarktischer Meteorite in der Ross Dependency geleitet hatte.ite in der Ross Dependency geleitet hatte. , 卡西迪冰川(英語:Cassidy Glacier)是南極洲的冰川,位於維多利亞地,長13公里、寬4公里,最終在德波冰原島峰和夸特梅因山脈西北端之間注入泰勒冰川上游,現時由南極條約體系管理。 , Cassidy Glacier (77°46′S 160°9′E / 77.76Cassidy Glacier (77°46′S 160°9′E / 77.767°S 160.150°E) is a glacier 7 nautical miles (13 km) long and 2 nautical miles (4 km) wide, flowing northeast into upper Taylor Glacier between Depot Nunatak and the northwest end of the Quartermain Mountains, in Victoria Land. The descriptive names "South-West Arm" and "South Arm" were applied to this glacier and to the part of Ferrar Glacier south of Knobhead, respectively, by the British National Antarctic Expedition, 1901–04. Subsequent mapping has shown that the glacier described here is part of the Taylor Glacier system. The glacier was named by the Advisory Committee on Antarctic Names in 1992 after William A. Cassidy, Department of Geology and Planetary Science, University of Pittsburgh, who in 13 field seasons, from 1976–90, led United States Antarctic Research Program teams in the investigation and collection of Antarctic meteorites from diverse sites through Victoria Land and southward to Lewis Cliff, adjacent to the Queen Alexandra Range.ff, adjacent to the Queen Alexandra Range.
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rdfs:comment Cassidy Glacier (77°46′S 160°9′E / 77.76Cassidy Glacier (77°46′S 160°9′E / 77.767°S 160.150°E) is a glacier 7 nautical miles (13 km) long and 2 nautical miles (4 km) wide, flowing northeast into upper Taylor Glacier between Depot Nunatak and the northwest end of the Quartermain Mountains, in Victoria Land. The descriptive names "South-West Arm" and "South Arm" were applied to this glacier and to the part of Ferrar Glacier south of Knobhead, respectively, by the British National Antarctic Expedition, 1901–04. Subsequent mapping has shown that the glacier described here is part of the Taylor Glacier system.here is part of the Taylor Glacier system. , Il ghiacciaio Cassidy è un ghiacciaio lungIl ghiacciaio Cassidy è un ghiacciaio lungo circa 13 km situato nella regione centro-occidentale della Dipendenza di Ross, in Antartide. Il ghiacciaio, il cui punto più alto si trova a circa 2000 m s.l.m., si trova in particolare tra le montagne di Quartermain, a est, e il , a ovest, nell'entroterra della costa di Scott, dove fluisce verso nord-est fino a unire il proprio flusso, a cui nel frattempo si è unito quello di altri ghiacciai come il Fitzpatrick e il Fireman, a quello del ghiacciaio Taylor.l Fireman, a quello del ghiacciaio Taylor. , Cassidy Glacier är en glaciär i Antarktis.Cassidy Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Nya Zeeland gör anspråk på området. Cassidy Glacier ligger 1 785 meter över havet. Terrängen runt Cassidy Glacier är kuperad åt sydost, men åt nordväst är den platt. Den högsta punkten i närheten är Marvin Nunatak, 2 090 meter över havet, 2,4 kilometer väster om Cassidy Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten.lkad. Det finns inga samhällen i närheten. , Der Cassidy-Gletscher ist ein rund 11 km lDer Cassidy-Gletscher ist ein rund 11 km langer langer und 3 km breiter Gletscher im ostantarktischen Viktorialand. Er fließt in nordöstlicher Richtung zwischen dem Depot-Nunatak und dem nordwestlichen Ende der Quartermain Mountains in den oberen Abschnitt des Taylor-Gletschers.en oberen Abschnitt des Taylor-Gletschers. , 卡西迪冰川(英語:Cassidy Glacier)是南極洲的冰川,位於維多利亞地,長13公里、寬4公里,最終在德波冰原島峰和夸特梅因山脈西北端之間注入泰勒冰川上游,現時由南極條約體系管理。
rdfs:label 卡西迪冰川 , Ghiacciaio Cassidy , Cassidy Glacier , Cassidy-Gletscher
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