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Statements

Subject Item
dbr:Campbell_Glacier
rdf:type
geo:SpatialThing yago:Object100002684 yago:Glacier109289331 yago:PhysicalEntity100001930 yago:IceMass109309292 yago:YagoGeoEntity yago:GeologicalFormation109287968 dbo:Place yago:YagoPermanentlyLocatedEntity yago:WikicatGlaciersOfVictoriaLand
rdfs:label
坎貝爾冰川 Campbell-Gletscher Campbell Glacier Ghiacciaio Campbell Campbell Glacier (glaciär i Antarktis, lat -74,42, long 164,37)
rdfs:comment
Der Campbell-Gletscher ist ein rund 100 km langer Gletscher im ostantarktischen Viktorialand. Er fließt vom Südende der Mesa Range in südöstlicher Richtung zwischen der Deep Freeze Range und Mount Melbourne und mündet an der Scott-Küste in Form der Campbell-Gletscherzunge (74° 36′ 0″ S, 164° 42′ 0″ O) in den nördlichen Abschnitt der Terra Nova Bay. Il ghiacciaio Campbell è un ghiacciaio lungo circa 110 km situato nella parte nord-occidentale della Dipendenza di Ross, nell'Antartide orientale. Il ghiacciaio, il cui punto più alto si trova a circa 2400 m s.l.m., nasce nell'entroterra della costa di Borchgrevink, dove si forma a sud della mesa Gair, e fluisce verso sud dividendo le montagne Southern Cross, a est, dalla dorsale Deep Freeze, a ovest, fino a entrare nella baia Terra Nova, nella costa di Scott, formando sulla baia una lingua glaciale lunga circa 25 km, che segna il confine oriental dell'.Lungo il suo percorso, il flusso del ghiacciaio Campbell è arricchito da quello di diversi altri ghiacciai, tra cui quello dei ghiacciai Rainey, Recoil, Rebuff e Capsize, che gli si uniscono da ovest, e quello del ghiacciaio Styx, che entra Campbell Glacier (74°25′S 164°22′E / 74.417°S 164.367°E) is a glacier, about 60 nautical miles (110 km) long, originating near the south end of Mesa Range and draining southeast between the Deep Freeze Range and Mount Melbourne to discharge into north Terra Nova Bay. The lower end of the glacier was observed by the Northern Party, led by Lieutenant Victor Campbell, Royal Navy, of the British Antarctic Expedition, 1910–13; it was named for the leader of this party. The extent of the glacier and its discharge into north Terra Nova Bay, rather than the Nansen Ice Sheet, was determined by United States and New Zealand survey parties to the area in 1961–62 and 1962–63. The steep bluff along the east side of the glacier is known as Hades Terrace, Bier Point is a projecting headland on the east 坎貝爾冰川（英語：Campbell Glacier）是南極洲的冰川，位於維多利亞地的斯科特海岸，全長約110公里，發源自梅薩山脈南端附近，最終注入特拉諾瓦灣北部。 Campbell Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Nya Zeeland gör anspråk på området. Campbell Glacier ligger 511 meter över havet. Terrängen runt Campbell Glacier är varierad. Den högsta punkten i närheten är 2 708 meter över havet, 11,5 kilometer nordost om Campbell Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten.
geo:lat
-74.41666412353516
geo:long
164.3666687011719
dcterms:subject
dbc:Glaciers_of_Scott_Coast
dbo:wikiPageID
29398467
dbo:wikiPageRevisionID
1105404254
dbo:wikiPageWikiLink
dbr:Victor_Campbell_(Royal_Navy_officer) dbr:Bier_Point dbr:United_States dbr:Suture_Bench dbr:Mount_Melbourne dbr:Glacier dbr:Rebuff_Glacier dbc:Glaciers_of_Scott_Coast dbr:Nansen_Ice_Sheet dbr:Terra_Nova_Bay dbr:New_Zealand dbr:Mesa_Range dbr:Deep_Freeze_Range dbr:Royal_Navy dbr:Browning_Pass_(Antarctica) dbr:British_Antarctic_Expedition,_1910–13 dbr:Hades_Terrace
owl:sameAs
n9:4fHUG dbpedia-zh:坎貝爾冰川 dbpedia-sv:Campbell_Glacier_(glaciär_i_Antarktis,_lat_-74,42,_long_164,37) dbpedia-nn:Campbellbreen dbpedia-it:Ghiacciaio_Campbell freebase:m.0dry6jy n22:Campbell_Glacier_(suba_sa_yelo_sa_Antartika,_lat_-74,42,_long_164,37) dbpedia-de:Campbell-Gletscher yago-res:Campbell_Glacier n26: wikidata:Q5028069
dbp:wikiPageUsesTemplate
dbt:Usgs-gazetteer dbt:ScottCoast-glacier-stub dbt:Reflist dbt:Coord dbt:Convert dbt:Glaciers_in_the_Antarctic dbt:Portal_bar
georss:point
-74.41666666666667 164.36666666666667
dbo:abstract
Il ghiacciaio Campbell è un ghiacciaio lungo circa 110 km situato nella parte nord-occidentale della Dipendenza di Ross, nell'Antartide orientale. Il ghiacciaio, il cui punto più alto si trova a circa 2400 m s.l.m., nasce nell'entroterra della costa di Borchgrevink, dove si forma a sud della mesa Gair, e fluisce verso sud dividendo le montagne Southern Cross, a est, dalla dorsale Deep Freeze, a ovest, fino a entrare nella baia Terra Nova, nella costa di Scott, formando sulla baia una lingua glaciale lunga circa 25 km, che segna il confine oriental dell'.Lungo il suo percorso, il flusso del ghiacciaio Campbell è arricchito da quello di diversi altri ghiacciai, tra cui quello dei ghiacciai Rainey, Recoil, Rebuff e Capsize, che gli si uniscono da ovest, e quello del ghiacciaio Styx, che entra nel suo flusso da nord-est. Campbell Glacier (74°25′S 164°22′E / 74.417°S 164.367°E) is a glacier, about 60 nautical miles (110 km) long, originating near the south end of Mesa Range and draining southeast between the Deep Freeze Range and Mount Melbourne to discharge into north Terra Nova Bay. The lower end of the glacier was observed by the Northern Party, led by Lieutenant Victor Campbell, Royal Navy, of the British Antarctic Expedition, 1910–13; it was named for the leader of this party. The extent of the glacier and its discharge into north Terra Nova Bay, rather than the Nansen Ice Sheet, was determined by United States and New Zealand survey parties to the area in 1961–62 and 1962–63. The steep bluff along the east side of the glacier is known as Hades Terrace, Bier Point is a projecting headland on the eastern side of Campbell Glacier. Der Campbell-Gletscher ist ein rund 100 km langer Gletscher im ostantarktischen Viktorialand. Er fließt vom Südende der Mesa Range in südöstlicher Richtung zwischen der Deep Freeze Range und Mount Melbourne und mündet an der Scott-Küste in Form der Campbell-Gletscherzunge (74° 36′ 0″ S, 164° 42′ 0″ O) in den nördlichen Abschnitt der Terra Nova Bay. Der untere Abschnitt des Gletschers wurde von der vom britischen Polarforscher Victor Campbell (1875–1956) geleiteten Nordgruppe der Terra-Nova-Expedition (1910–1913) entdeckt. US-amerikanische und neuseeländische Landvermessungen erfassten in den Jahren von 1961 bis 1964 die geografische Ausdehnung des Gletschergebiets. Diese führten zur Widerlegung Campbells irrtümlicher Annahme, der Gletscher münde statt in die Terra Nova Bay in die Nansen-Eistafel. Campbell Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Nya Zeeland gör anspråk på området. Campbell Glacier ligger 511 meter över havet. Terrängen runt Campbell Glacier är varierad. Den högsta punkten i närheten är 2 708 meter över havet, 11,5 kilometer nordost om Campbell Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. 坎貝爾冰川（英語：Campbell Glacier）是南極洲的冰川，位於維多利亞地的斯科特海岸，全長約110公里，發源自梅薩山脈南端附近，最終注入特拉諾瓦灣北部。
gold:hypernym
dbr:Glacier
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wikipedia-en:Campbell_Glacier?oldid=1105404254&ns=0
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geo:geometry
POINT(164.36666870117 -74.416664123535)