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Statements

Subject Item
dbr:Michigan_Plateau
rdf:type
yago:GeologicalFormation109287968 geo:SpatialThing yago:PhysicalEntity100001930 yago:NaturalElevation109366317 owl:Thing yago:WikicatPlateausOfAntarctica yago:YagoPermanentlyLocatedEntity yago:YagoGeoEntity yago:Tableland109453008 dbo:Place yago:Object100002684 yago:Highland109302616 dbo:Location schema:Place
rdfs:label
Michigan Plateau 密歇根高原 Michigan-Plateau Michigan Plateau Michigan Plateau
rdfs:comment
Das Michigan-Plateau ist ein eisbedecktes, wellenförmiges Hochplateau von rund 50 km Länge im westantarktischen Marie-Byrd-Land. Es erhebt sich bis zu 3000 m hoch an der Westflanke des Reedy-Gletschers. Die Nord- und Ostseite sind durch das steilwandige Watson Escarpment markiert. Die West- und Südflanke steigen bis auf das Niveau des zentralen Polarplateaus an. Michigan Plateau (86°8′S 133°30′W / 86.133°S 133.500°W) is an undulating ice-covered plateau, 30 nautical miles (56 km) long, which rises to 3,000 metres (10,000 ft) at the western side of Reedy Glacier, Antarctica. The northern and eastern sides of the plateau are marked by the steep Watson Escarpment; the western and southern sides grade gradually to the elevation of the interior ice. It was mapped by the United States Geological Survey from ground surveys and U.S. Navy aerial photography, 1960–64, and was named by the Advisory Committee on Antarctic Names after the University of Michigan at Ann Arbor, which has sent numerous research personnel to work in Antarctica. Michigan Plateau är en platå i Antarktis. Den ligger i den centrala delen av kontinenten. Inget land gör anspråk på området. Il Michigan Plateau è un altopiano antartico, ondulato e coperto di ghiaccio, lungo 56 km, situato a circa 3.000 m di altitudine sul fianco occidentale del Ghiacciaio Reedy, nei Monti della Regina Maud, in Antartide. I fianchi settentrionale e orientale del Michigan Plateau sono caratterizzati dalle ripide pareti rocciose del Watson Escarpment; invece i fianchi occidentale e meridionale degradano dolcemente fino all'altezza del ghiaccio dell'Altopiano Antartico. 密歇根高原（英語：Michigan Plateau）是南極洲的高原，位於瑪麗伯德地，長56公里，處於里迪冰川西面，海拔高度3,000米，根據美國地質調查局的測量和美國海軍的空中照片被繪入地圖。
geo:lat
-86.13333129882812
geo:long
-133.5
dbo:location
dbr:Antarctica dbr:West_Antarctica
dcterms:subject
dbc:Plateaus_of_Antarctica dbc:University_of_Michigan dbc:Landforms_of_Marie_Byrd_Land
dbo:wikiPageID
29558025
dbo:wikiPageRevisionID
1089576570
dbo:wikiPageWikiLink
dbr:United_States_Geological_Survey dbr:Reedy_Glacier dbr:Advisory_Committee_on_Antarctic_Names dbc:Plateaus_of_Antarctica dbc:University_of_Michigan dbc:Landforms_of_Marie_Byrd_Land dbr:U.S._Navy dbr:Kirby_Cone dbr:Kivi_Peak dbr:University_of_Michigan_at_Ann_Arbor dbr:Watson_Escarpment
owl:sameAs
n5:Michigan_Plateau dbpedia-it:Michigan_Plateau dbpedia-nn:Michigan_Plateau dbpedia-de:Michigan-Plateau n17:4rwVn yago-res:Michigan_Plateau wikidata:Q6837643 dbpedia-zh:密歇根高原 dbpedia-sv:Michigan_Plateau n26: freebase:m.0ds5y95
dbp:wikiPageUsesTemplate
dbt:Reflist dbt:Convert dbt:Usgs-gazetteer dbt:Coord dbt:MarieByrdLand-geo-stub
georss:point
-86.13333333333334 -133.5
dbo:abstract
Michigan Plateau är en platå i Antarktis. Den ligger i den centrala delen av kontinenten. Inget land gör anspråk på området. Il Michigan Plateau è un altopiano antartico, ondulato e coperto di ghiaccio, lungo 56 km, situato a circa 3.000 m di altitudine sul fianco occidentale del Ghiacciaio Reedy, nei Monti della Regina Maud, in Antartide. I fianchi settentrionale e orientale del Michigan Plateau sono caratterizzati dalle ripide pareti rocciose del Watson Escarpment; invece i fianchi occidentale e meridionale degradano 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 del Michigan che hanno inviato numerosi studiosi a compiere ricerche in Antartide. Das Michigan-Plateau ist ein eisbedecktes, wellenförmiges Hochplateau von rund 50 km Länge im westantarktischen Marie-Byrd-Land. Es erhebt sich bis zu 3000 m hoch an der Westflanke des Reedy-Gletschers. Die Nord- und Ostseite sind durch das steilwandige Watson Escarpment markiert. Die West- und Südflanke steigen bis auf das Niveau des zentralen Polarplateaus an. Kartografisch erfasst wurde das Gebiet durch den United States Geological Survey und durch Luftaufnahmen der United States Navy aus den Jahren 1960 bis 1964. Das Advisory Committee on Antarctic Names benannte es 1967 nach der University of Michigan, die zahlreiche Wissenschaftler für Forschungsarbeiten in Antarktika entsendet hatte. Michigan Plateau (86°8′S 133°30′W / 86.133°S 133.500°W) is an undulating ice-covered plateau, 30 nautical miles (56 km) long, which rises to 3,000 metres (10,000 ft) at the western side of Reedy Glacier, Antarctica. The northern and eastern sides of the plateau are marked by the steep Watson Escarpment; the western and southern sides grade gradually to the elevation of the interior ice. It was mapped by the United States Geological Survey from ground surveys and U.S. Navy aerial photography, 1960–64, and was named by the Advisory Committee on Antarctic Names after the University of Michigan at Ann Arbor, which has sent numerous research personnel to work in Antarctica. 密歇根高原（英語：Michigan Plateau）是南極洲的高原，位於瑪麗伯德地，長56公里，處於里迪冰川西面，海拔高度3,000米，根據美國地質調查局的測量和美國海軍的空中照片被繪入地圖。
gold:hypernym
dbr:Plateau
prov:wasDerivedFrom
wikipedia-en:Michigan_Plateau?oldid=1089576570&ns=0
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1106
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dbr:Marie_Byrd_Land
foaf:isPrimaryTopicOf
wikipedia-en:Michigan_Plateau
geo:geometry
POINT(-133.5 -86.133331298828)