Horlick Ice Stream (original) (raw)

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Horlick Ice Stream (85°17′S 132°00′W / 85.283°S 132.000°W) is a large ice stream on the featureless ice surface to the north of the main mass of the Horlick Mountains of Antarctica, draining west-southwestward, parallel to these mountains, to enter the lower portion of the Reedy Glacier. It was mapped by the U.S. Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names in association with the Horlick Mountains.

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dbo:abstract Der Horlick-Eisstrom ist ein großer Eisstrom im westantarktischen Marie-Byrd-Land. Im strukturlosen Norden des Hauptmassivs der Horlick Mountains fließt er parallel zu diesen in westsüdwestlicher Richtung zum unteren Abschnitt des Reedy-Gletschers. Das Gebiet wurde vom 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 ihn 1967 in Verbindung mit den Horlick Mountains nach dem Unternehmer (1846–1936), einem Sponsoren der zweiten Antarktisexpedition (1933–1935) des US-amerikanischen Polarforschers Richard Evelyn Byrd. (de) Horlick Ice Stream (85°17′S 132°00′W / 85.283°S 132.000°W) is a large ice stream on the featureless ice surface to the north of the main mass of the Horlick Mountains of Antarctica, draining west-southwestward, parallel to these mountains, to enter the lower portion of the Reedy Glacier. It was mapped by the U.S. Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names in association with the Horlick Mountains. (en) Il flusso di ghiaccio Horlick è un flusso di ghiaccio lungo oltre 100 km situato in Antartide, dove si origina, in particolare, nell'entroterra della Terra di Marie Byrd. Situato nella piatta pianura glaciale sita a nord del blocco dei monti Horlick, il flusso glaciale Horlick si muove verso ovest-sud-ovest parallelamente all'estensione dei suddetti monti e lungo il suo percorso viene arricchito dal flusso glaciale Shimizu e da altri suoi tributari, come il ghiacciaio Davisville, fino ad andare ad alimentare il ghiacciaio Reedy, nella parte orientale del territorio della Dipendenza di Ross. (it) 霍利克冰流(英語:Horlick Ice Stream),是南極洲的冰流,位於瑪麗伯德地,美國地質調查局根據測量和美國海軍拍攝的空中照片繪入地圖,現時由南極條約體系管理。 (zh)
dbo:locatedInArea dbr:Marie_Byrd_Land
dbo:location dbr:Antarctica dbr:Marie_Byrd_Land dbr:West_Antarctica
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dbo:wikiPageLength 1730 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID 1085646911 (xsd:integer)
dbo:wikiPageWikiLink dbc:West_Antarctica dbr:List_of_glaciers_in_the_Antarctic dbr:Glaciology dbr:Antarctica dbr:Horlick_Mountains dbr:Ice_stream dbr:List_of_Antarctic_ice_streams dbc:Ice_streams_of_Antarctica dbr:Advisory_Committee_on_Antarctic_Names dbr:Reedy_Glacier dbr:Marie_Byrd_Land dbr:U.S._Geological_Survey
dbp:location dbr:Marie_Byrd_Land
dbp:mapCaption Location of Horlick Ice Stream in Antarctica (en)
dbp:name Horlick Ice Stream (en)
dbp:status unknown (en)
dbp:terminus dbr:Reedy_Glacier
dbp:thickness unknown (en)
dbp:wikiPageUsesTemplate dbt:Glaciers_in_the_Antarctic dbt:Usgs-gazetteer dbt:Coord dbt:Portal_bar dbt:Reflist dbt:Short_description dbt:Glaciology-stub dbt:MarieByrdLand-geo-stub dbt:Infobox_glacier
dcterms:subject dbc:West_Antarctica dbc:Ice_streams_of_Antarctica
gold:hypernym dbr:Stream
georss:point -85.28333333333333 -132.0
rdf:type owl:Thing dbo:Place dbo:Location schema:Place dbo:NaturalPlace dbo:Glacier geo:SpatialThing dbo:River wikidata:Q35666 yago:BodyOfWater109225146 yago:PhysicalEntity100001930 yago:WikicatIceStreamsOfAntarctica yago:YagoGeoEntity yago:YagoPermanentlyLocatedEntity yago:Stream109448361 yago:Thing100002452
rdfs:comment Horlick Ice Stream (85°17′S 132°00′W / 85.283°S 132.000°W) is a large ice stream on the featureless ice surface to the north of the main mass of the Horlick Mountains of Antarctica, draining west-southwestward, parallel to these mountains, to enter the lower portion of the Reedy Glacier. It was mapped by the U.S. Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names in association with the Horlick Mountains. (en) Il flusso di ghiaccio Horlick è un flusso di ghiaccio lungo oltre 100 km situato in Antartide, dove si origina, in particolare, nell'entroterra della Terra di Marie Byrd. Situato nella piatta pianura glaciale sita a nord del blocco dei monti Horlick, il flusso glaciale Horlick si muove verso ovest-sud-ovest parallelamente all'estensione dei suddetti monti e lungo il suo percorso viene arricchito dal flusso glaciale Shimizu e da altri suoi tributari, come il ghiacciaio Davisville, fino ad andare ad alimentare il ghiacciaio Reedy, nella parte orientale del territorio della Dipendenza di Ross. (it) 霍利克冰流(英語:Horlick Ice Stream),是南極洲的冰流,位於瑪麗伯德地,美國地質調查局根據測量和美國海軍拍攝的空中照片繪入地圖,現時由南極條約體系管理。 (zh) Der Horlick-Eisstrom ist ein großer Eisstrom im westantarktischen Marie-Byrd-Land. Im strukturlosen Norden des Hauptmassivs der Horlick Mountains fließt er parallel zu diesen in westsüdwestlicher Richtung zum unteren Abschnitt des Reedy-Gletschers. (de)
rdfs:label Horlick-Eisstrom (de) Horlick Ice Stream (en) Flusso di ghiaccio Horlick (it) 霍利克冰流 (zh)
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geo:lat -85.283333 (xsd:float)
geo:long -132.000000 (xsd:float)
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foaf:name Horlick Ice Stream (en)
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