Louisville Ridge (original) (raw)
Louisville itsaspeko mendilerroa, Ozeano Barearen hegomendebaldean dagoen 70 itsaspeko mendi baino gehiagoz osatutako itsaspeko mendilerro bat da. Lurreko itsaspeko mendilerrorik luzeenetako bat da, 4300 kilometroz hedatzen baita, Pazifiko-Antartika dortsaletik ekialde-iparrekialdean, Tonga-Kermadeceko fosaraino, non azpian subduzitzen den, Pazifiko plakako zati bezala. Mendilerroa, Pazifiko plakaren gaineko mugimenduaren ondorioz eratua dago.
| Property | Value |
|---|---|
| dbo:abstract | Louisville itsaspeko mendilerroa, Ozeano Barearen hegomendebaldean dagoen 70 itsaspeko mendi baino gehiagoz osatutako itsaspeko mendilerro bat da. Lurreko itsaspeko mendilerrorik luzeenetako bat da, 4300 kilometroz hedatzen baita, Pazifiko-Antartika dortsaletik ekialde-iparrekialdean, Tonga-Kermadeceko fosaraino, non azpian subduzitzen den, Pazifiko plakako zati bezala. Mendilerroa, Pazifiko plakaren gaineko mugimenduaren ondorioz eratua dago. (eu) The Louisville Ridge, also known as the Louisville Seamount Chain, is an underwater chain of over 70 seamounts located in the Southwest portion of the Pacific Ocean. As one of the longest seamount chains on Earth it stretches some 4,300 km (2,700 mi) from the Pacific-Antarctic Ridge northwest to the Tonga-Kermadec Trench, where it subducts under the Indo-Australian Plate as part of the Pacific Plate. The chain may have been formed by movement of the Pacific Plate over the Louisville hotspot or by leakage of magma from the shallow mantle up through the Eltanin fracture zone, which it follows closely. Depth-sounding data first revealed the existence of the seamount chain in 1972. (en) La chaîne sous-marine Louisville est une chaîne de plus de 70 monts sous-marins située dans le Sud-Ouest de l'océan Pacifique. Elle est l'une des plus longues chaînes de montagnes sous-marines sur Terre, s'étendant sur quelque 4 300 km à partir de la dorsale Pacifique-Antarctique aux fosses Tonga-Kermadec, où il sous-conduit la plaque indo-australienne, partie intégrante de la plaque pacifique. Son existence fut révélée en 1972 grâce aux données d'un sondage à main. (fr) La catena sottomarina di Louisville è una formazione montuosa sottomarina situata nella regione sud occidentale dell'Oceano Pacifico e costituita da una serie di più di 70 montagne sottomarine. (it) ルイビル海山列（るいびるかいざんれつ 英語：Louisville seamount chain）は、太平洋南西部にある、70以上の海山からなる列。地球上最長の海山列の一つであり、長さはおよそ4300kmに達する 。太平洋南極海嶺から東北東にトンガ・ケルマデック海溝まで伸び、そこで太平洋プレートの一部としてインド・オーストラリアプレートに沈み込んでいる。この海山列は、ルイビルホットスポット上を太平洋プレートが移動することで形成された。 ルイビル海山列の存在は1972年に明らかになった。 (ja) |
| dbo:thumbnail | wiki-commons:Special:FilePath/Louisville_seamount_chain_-_bathymetry.jpg?width=300 |
| dbo:wikiPageExternalLink | http://iodp.tamu.edu/scienceops/expeditions/louisville_seamounts.html https://www.bodc.ac.uk/data/information_and_inventories/cruise_inventory/report/sonne215.pdf |
| dbo:wikiPageID | 16987262 (xsd:integer) |
| dbo:wikiPageLength | 4834 (xsd:nonNegativeInteger) |
| dbo:wikiPageRevisionID | 1065958274 (xsd:integer) |
| dbo:wikiPageWikiLink | dbr:Hollister_Ridge dbr:Depth_sounding dbr:Indo-Australian_Plate dbr:Louisville_hotspot dbr:Seamount dbc:Seamounts_of_the_Pacific_Ocean dbr:Hotspot_(geology) dbr:Kermadec_Trench dbr:Pacific-Antarctic_Ridge dbr:Tonga_Trench dbr:Osbourn_Seamount dbr:Pacific_Ocean dbr:Pacific_Plate dbc:Guyots dbc:Oceanography dbc:Seamount_chains dbr:Integrated_Ocean_Drilling_Program dbr:RV_Sonne dbc:Hotspot_tracks dbr:Louisville_Seamount dbr:Burton_Seamount dbr:Currituck_Seamount dbr:Danseur_Seamount dbr:Darvin_Guyot dbr:File:Louisville_seamount_chain_-_bathymetry.jpg dbr:Forde_Seamount dbr:Pierson_Seamount dbr:Rumyantsev_Seamount dbr:Seafox_Seamount dbr:Trobriant_Seamount dbr:Valerie_Guyot dbr:Vostok_Seamount |
| dbp:discovered | 1972 (xsd:integer) |
| dbp:location | Southwest Pacific Ocean (en) |
| dbp:mapCaption | The Louisville Ridge stretches diagonally across this bathymetric map of the southwest Pacific Ocean. (en) |
| dbp:name | Louisville Ridge (en) |
| dbp:summitArea | length: (en) |
| dbp:type | dbr:Seamount |
| dbp:volcanicGroup | dbr:Louisville_hotspot |
| dbp:wikiPageUsesTemplate | dbt:Infobox_Seamount dbt:Convert dbt:Coord dbt:Reflist dbt:Short_description |
| dcterms:subject | dbc:Seamounts_of_the_Pacific_Ocean dbc:Guyots dbc:Oceanography dbc:Seamount_chains dbc:Hotspot_tracks |
| georss:point | -38.27 -167.92 |
| rdf:type | geo:SpatialThing |
| rdfs:comment | Louisville itsaspeko mendilerroa, Ozeano Barearen hegomendebaldean dagoen 70 itsaspeko mendi baino gehiagoz osatutako itsaspeko mendilerro bat da. Lurreko itsaspeko mendilerrorik luzeenetako bat da, 4300 kilometroz hedatzen baita, Pazifiko-Antartika dortsaletik ekialde-iparrekialdean, Tonga-Kermadeceko fosaraino, non azpian subduzitzen den, Pazifiko plakako zati bezala. Mendilerroa, Pazifiko plakaren gaineko mugimenduaren ondorioz eratua dago. (eu) La chaîne sous-marine Louisville est une chaîne de plus de 70 monts sous-marins située dans le Sud-Ouest de l'océan Pacifique. Elle est l'une des plus longues chaînes de montagnes sous-marines sur Terre, s'étendant sur quelque 4 300 km à partir de la dorsale Pacifique-Antarctique aux fosses Tonga-Kermadec, où il sous-conduit la plaque indo-australienne, partie intégrante de la plaque pacifique. Son existence fut révélée en 1972 grâce aux données d'un sondage à main. (fr) La catena sottomarina di Louisville è una formazione montuosa sottomarina situata nella regione sud occidentale dell'Oceano Pacifico e costituita da una serie di più di 70 montagne sottomarine. (it) ルイビル海山列（るいびるかいざんれつ 英語：Louisville seamount chain）は、太平洋南西部にある、70以上の海山からなる列。地球上最長の海山列の一つであり、長さはおよそ4300kmに達する 。太平洋南極海嶺から東北東にトンガ・ケルマデック海溝まで伸び、そこで太平洋プレートの一部としてインド・オーストラリアプレートに沈み込んでいる。この海山列は、ルイビルホットスポット上を太平洋プレートが移動することで形成された。 ルイビル海山列の存在は1972年に明らかになった。 (ja) The Louisville Ridge, also known as the Louisville Seamount Chain, is an underwater chain of over 70 seamounts located in the Southwest portion of the Pacific Ocean. As one of the longest seamount chains on Earth it stretches some 4,300 km (2,700 mi) from the Pacific-Antarctic Ridge northwest to the Tonga-Kermadec Trench, where it subducts under the Indo-Australian Plate as part of the Pacific Plate. The chain may have been formed by movement of the Pacific Plate over the Louisville hotspot or by leakage of magma from the shallow mantle up through the Eltanin fracture zone, which it follows closely. (en) |
| rdfs:label | Louisville itsaspeko mendilerroa (eu) Catena sottomarina di Louisville (it) Chaîne sous-marine Louisville (fr) Louisville Ridge (en) ルイビル海山列 (ja) |
| owl:sameAs | wikidata:Louisville Ridge dbpedia-eu:Louisville Ridge dbpedia-fr:Louisville Ridge dbpedia-it:Louisville Ridge dbpedia-ja:Louisville Ridge https://global.dbpedia.org/id/2kCqC |
| geo:geometry | POINT(-167.91999816895 -38.270000457764) |
| geo:lat | -38.270000 (xsd:float) |
| geo:long | -167.919998 (xsd:float) |
| prov:wasDerivedFrom | wikipedia-en:Louisville_Ridge?oldid=1065958274&ns=0 |
| foaf:depiction | wiki-commons:Special:FilePath/Louisville_seamount_chain_-_bathymetry.jpg |
| foaf:isPrimaryTopicOf | wikipedia-en:Louisville_Ridge |
| is dbo:wikiPageDisambiguates of | dbr:Louisville_(disambiguation) |
| is dbo:wikiPageRedirects of | dbr:Louisville_seamount_chain dbr:Louisville_Seamount |
| is dbo:wikiPageWikiLink of | dbr:Louisville_seamount_chain dbr:Intraplate_volcanism dbr:Timeline_of_volcanism_on_Earth dbr:1977_Tonga_earthquake dbr:Geology_of_the_Pacific_Ocean dbr:Louisville_hotspot dbr:Ontong_Java_Plateau dbr:Hotspot_(geology) dbr:Kermadec_Trench dbr:Mantle_plume dbr:Pacific-Antarctic_Ridge dbr:Tonga_Trench dbr:Osbourn_Seamount dbr:Pacific_Ocean dbr:Integrated_Ocean_Drilling_Program dbr:Tonga-Kermadec_Ridge dbr:Louisville_(disambiguation) dbr:Outline_of_oceanography dbr:Louisville_Seamount |
| is dbp:volcanicGroup of | dbr:Osbourn_Seamount |
| is foaf:primaryTopic of | wikipedia-en:Louisville_Ridge |
