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Statements

Subject Item
dbr:Astrid_Ridge
rdf:type
yago:Object100002684 yago:Ridge109409512 dbo:Location geo:SpatialThing wikidata:Q8502 yago:GeologicalFormation109287968 owl:Thing schema:Place yago:YagoPermanentlyLocatedEntity dbo:Mountain yago:WikicatRidgesOfQueenMaudLand schema:Mountain yago:YagoGeoEntity yago:PhysicalEntity100001930 yago:NaturalElevation109366317 dbo:NaturalPlace dbo:Place
rdfs:label
Astrid Ridge Astrid Ridge Astrid Ridge
rdfs:comment
Astrid Ridge är en undervattensås i Antarktis. Den ligger i havet utanför Östantarktis. Norge gör anspråk på området. Der Astrid Ridge (englisch; von ridge „Erhöhung, Kamm, Rücken, Höhenrücken“) ist ein Tiefseerücken im Südlichen Ozean vor der Prinzessin-Ragnhild-Küste des ostantarktischen Königin-Maud-Lands. Namensgeber ist die belgische Königin Astrid (1905–1935), Ehefrau von Leopold III. Das US-amerikanische (ACUF) bestätigte die Benennung im Juni 1988. Astrid Ridge is an undersea ridge on the continental margin of Dronning Maud Land, East Antarctica. It is present on the GEBCO 5th edition charts. The name was approved by the Advisory Committee for Undersea Features in June 1987. The ocean along the continental margin of Dronning Maud Land, the Riiser-Larsen and Lazarev seas, are dominated by three topographic features: Astrid Ridge, Maud Rise, a large volcanic plateau in the Lazarev Sea (3°E, 65°S), and (33.5°E), probably underlain by continental crust.
foaf:name
Astrid Ridge
dbp:name
Astrid Ridge
geo:lat
-68.0
geo:long
12.0
dct:subject
dbc:Ridges_of_Queen_Maud_Land dbc:Princess_Astrid_Coast
dbo:wikiPageID
16490543
dbo:wikiPageRevisionID
1075447231
dbo:wikiPageWikiLink
dbr:Maud_Rise dbr:Continental_crust dbr:Riiser-Larsen_Sea dbc:Ridges_of_Queen_Maud_Land dbr:Dronning_Maud_Land dbr:Advisory_Committee_for_Undersea_Features dbr:Magnetic_anomaly dbr:East_Antarctica dbr:Lazarev_Sea dbr:Oceanic_crust dbr:Gunnerus_Ridge dbr:Undersea_ridge dbr:Gondwana dbc:Princess_Astrid_Coast dbr:GEBCO dbr:Mozambique_Basin
dbo:wikiPageExternalLink
n12:242073718
owl:sameAs
n16:Astrid_Ridge n18: wikidata:Q4811441 n20:4TZ2Z freebase:m.03y8lqd yago-res:Astrid_Ridge dbpedia-sv:Astrid_Ridge dbpedia-de:Astrid_Ridge
dbp:wikiPageUsesTemplate
dbt:Cite_journal dbt:Coord dbt:Infobox_mountain dbt:Refend dbt:Reflist dbt:Refbegin dbt:Short_description dbt:PrincessAstridCoast-geo-stub
dbp:mapAlt
Map of Antarctica
dbp:mapRelief
1
dbp:mapSize
256
georss:point
-68.0 12.0
dbo:abstract
Der Astrid Ridge (englisch; von ridge „Erhöhung, Kamm, Rücken, Höhenrücken“) ist ein Tiefseerücken im Südlichen Ozean vor der Prinzessin-Ragnhild-Küste des ostantarktischen Königin-Maud-Lands. Namensgeber ist die belgische Königin Astrid (1905–1935), Ehefrau von Leopold III. Das US-amerikanische (ACUF) bestätigte die Benennung im Juni 1988. Astrid Ridge är en undervattensås i Antarktis. Den ligger i havet utanför Östantarktis. Norge gör anspråk på området. Astrid Ridge is an undersea ridge on the continental margin of Dronning Maud Land, East Antarctica. It is present on the GEBCO 5th edition charts. The name was approved by the Advisory Committee for Undersea Features in June 1987. The ocean along the continental margin of Dronning Maud Land, the Riiser-Larsen and Lazarev seas, are dominated by three topographic features: Astrid Ridge, Maud Rise, a large volcanic plateau in the Lazarev Sea (3°E, 65°S), and (33.5°E), probably underlain by continental crust. Astrid Ridge, extending from 65°S to the Antarctic margin and located between 9°E and 17°E, forms the eastern border of the Lazarev Sea and the western border of the Riiser-Larsen Sea. It is divided into two parts by the Astrid Fracture Zone: south of 67°S Astrid Ridge stretches N-S while the northern part follows the SW—NE direction of the fracture zone. The geological evolution of the Astrid Ridge remains enigmatic. The Riiser-Larsen Sea is a conjugate basin to the (in the ocean east of southern Africa) and the two once formed the first ocean to open during the break-up of Gondwana.Astrid Ridge is a large volcanic features closely related to this 160 Ma break-up during which oceanic crust began to form in the Riiser-Larsen Sea. West of Astrid Ridge, however, neither oceanic crust nor magnetic anomalies have been found and this area is therefore interpreted as stretched continental crust and Astrid Ridge as a former continental margin created by volcanism during the break-up.
gold:hypernym
dbr:Name
prov:wasDerivedFrom
wikipedia-en:Astrid_Ridge?oldid=1075447231&ns=0
dbo:wikiPageLength
3318
foaf:isPrimaryTopicOf
wikipedia-en:Astrid_Ridge
geo:geometry
POINT(12 -68)