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Statements

Subject Item
dbr:California_Plateau
rdf:type
yago:Object100002684 dbo:Place yago:Tableland109453008 dbo:Location yago:Highland109302616 yago:NaturalElevation109366317 geo:SpatialThing yago:YagoGeoEntity yago:GeologicalFormation109287968 owl:Thing yago:YagoPermanentlyLocatedEntity schema:Place yago:WikicatPlateausOfAntarctica yago:PhysicalEntity100001930
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California Plateau 加利福尼亞高原 California Plateau California Plateau California-Plateau
rdfs:comment
California Plateau (86°4′S 145°10′W / 86.067°S 145.167°W) is an undulating ice-covered plateau, 30 nautical miles (56 km) long and from 2 to 12 nautical miles (4 to 22 km) wide, which rises to 3,000 metres (10,000 ft) at the eastern side of Scott Glacier. The plateau reaches a maximum height of 3,275 metres (10,745 ft) in Mount Blackburn at the southern end. The northwestern side of the plateau is marked by the steep rock cliffs of Watson Escarpment; the southeastern side grades gradually to the elevation of the interior ice. It was mapped by the United States Geological Survey from ground surveys and from U.S. Navy aerial photography, 1960–64, and named by the Advisory Committee on Antarctic Names for the several branches of the University of California which have sent numerous research California Plateau är en platå i Antarktis. Den ligger i den centrala delen av kontinenten. Inget land gör anspråk på området. Das California-Plateau ist eine etwa 3000 m hohe, wellige und eisbedeckte Hochebene im westantarktischen Marie-Byrd-Land. Sie liegt an der Ostflanke des Scott-Gletschers mit einer Ausdehnung von etwa 50 km Länge und zwischen 3 und 20 km Breite. Am südlichen Ende des Plateaus erhebt sich Mount Blackburn mit einer Höhe von 3275 m. Die Nordwestseite ist gekennzeichnet durch die steilen Kliffs des Watson Escarpment, die Südostseite hingegen fällt sanft auf das Niveau des zentralen Polarplateaus ab. Il California Plateau è un altopiano antartico, ondulato e coperto di ghiaccio, lungo 56 km e largo da 4 a 22 km, situato a circa 3.000 m di altitudine sul fianco orientale del Ghiacciaio Scott. Il plateau raggiunge un'altezza massima di 3.275 m all'estremità meridionale del Monte Blackburn, nei Monti della Regina Maud, in Antartide. Il fianco nordoccidentale del California Plateau è caratterizzato dalle ripide pareti rocciose del Watson Escarpment; invece il fianco sudorientale degrada dolcemente fino all'altezza del ghiaccio dell'Altopiano Antartico. 加利福尼亞高原（英語：California Plateau）是南極洲的高原，長56公里、寬4至22公里，最高點是海拔高度3,275米的布萊克本山，西北面以沃森海崖為界，該高原以加利福尼亞大學命名。
geo:lat
-86.06666564941406
geo:long
-145.1666717529297
dbo:location
dbr:West_Antarctica dbr:Antarctica
dcterms:subject
dbc:Plateaus_of_Antarctica dbc:Landforms_of_Marie_Byrd_Land
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dbo:wikiPageRevisionID
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dbo:wikiPageWikiLink
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dbo:abstract
Il California Plateau è un altopiano antartico, ondulato e coperto di ghiaccio, lungo 56 km e largo da 4 a 22 km, situato a circa 3.000 m di altitudine sul fianco orientale del Ghiacciaio Scott. Il plateau raggiunge un'altezza massima di 3.275 m all'estremità meridionale del Monte Blackburn, nei Monti della Regina Maud, in Antartide. Il fianco nordoccidentale del California Plateau è caratterizzato dalle ripide pareti rocciose del Watson Escarpment; invece il fianco sudorientale degrada dolcemente fino all'altezza del ghiaccio dell'Altopiano Antartico. Il plateau è stato mappato dall'United States Geological Survey (USGS) sulla base di rilevazioni e foto aeree scattate dalla U.S. Navy nel periodo 1960-64. La denominazione è stata assegnata dall'Advisory Committee on Antarctic Names (US-ACAN) in onore dei molti dipartimenti dell'Università della California che hanno inviato numerosi studiosi a compiere ricerche in Antartide. Das California-Plateau ist eine etwa 3000 m hohe, wellige und eisbedeckte Hochebene im westantarktischen Marie-Byrd-Land. Sie liegt an der Ostflanke des Scott-Gletschers mit einer Ausdehnung von etwa 50 km Länge und zwischen 3 und 20 km Breite. Am südlichen Ende des Plateaus erhebt sich Mount Blackburn mit einer Höhe von 3275 m. Die Nordwestseite ist gekennzeichnet durch die steilen Kliffs des Watson Escarpment, die Südostseite hingegen fällt sanft auf das Niveau des zentralen Polarplateaus ab. Das Gebiet wurde durch Vermessungsarbeiten des United States Geological Survey und mithilfe von Luftaufnahmen der United States Navy von 1960 bis 1964 kartografisch erfasst. Das Advisory Committee on Antarctic Names benannte es 1967 zu Ehren der University of California, von der zahlreiche in Antarktika tätige Wissenschaftler unterschiedlicher Forschungsdisziplinen stammten. California Plateau (86°4′S 145°10′W / 86.067°S 145.167°W) is an undulating ice-covered plateau, 30 nautical miles (56 km) long and from 2 to 12 nautical miles (4 to 22 km) wide, which rises to 3,000 metres (10,000 ft) at the eastern side of Scott Glacier. The plateau reaches a maximum height of 3,275 metres (10,745 ft) in Mount Blackburn at the southern end. The northwestern side of the plateau is marked by the steep rock cliffs of Watson Escarpment; the southeastern side grades gradually to the elevation of the interior ice. It was mapped by the United States Geological Survey from ground surveys and from U.S. Navy aerial photography, 1960–64, and named by the Advisory Committee on Antarctic Names for the several branches of the University of California which have sent numerous researchers to work in Antarctica. 加利福尼亞高原（英語：California Plateau）是南極洲的高原，長56公里、寬4至22公里，最高點是海拔高度3,275米的布萊克本山，西北面以沃森海崖為界，該高原以加利福尼亞大學命名。 California Plateau är en platå i Antarktis. Den ligger i den centrala delen av kontinenten. Inget land gör anspråk på området.
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dbr:Plateau
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