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.
Attributes | Values |
---|
rdf:type
| |
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)
|
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)
|
name
| |
geo:lat
| |
geo:long
| |
foaf:depiction
| |
dcterms:subject
| |
Wikipage page ID
| |
Wikipage revision ID
| |
Link from a Wikipage to another Wikipage
| |
Link from a Wikipage to an external page
| |
sameAs
| |
summit area
| |
volcanic group
| |
dbp:wikiPageUsesTemplate
| |
thumbnail
| |
discovered
| |
location
| - Southwest Pacific Ocean (en)
|
map caption
| - The Louisville Ridge stretches diagonally across this bathymetric map of the southwest Pacific Ocean. (en)
|
type
| |
georss:point
| |
has 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)
|
prov:wasDerivedFrom
| |
page length (characters) of wiki page
| |
foaf:isPrimaryTopicOf
| |
geo:geometry
| - POINT(-167.91999816895 -38.270000457764)
|
is Link from a Wikipage to another Wikipage
of | |