About: Jemez Lineament

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The Jemez Lineament is a chain of late Cenozoic volcanic fields, 800 kilometers (500 mi) long, reaching from the Springerville and White Mountains volcanic fields in East-Central Arizona to the Raton-Clayton volcanic field in Northeastern New Mexico.

Attributes	Values
rdf:type	yago:WikicatVolcanoesOfNewMexico yago:Abstraction100002137 yago:AmorphousShape113867492 yago:Attribute100024264 yago:Crack109258715 yago:GeologicalFormation109287968 yago:Location100027167 yago:Mountain109359803 yago:NaturalElevation109366317 yago:Object100002684 yago:Opening109379111 yago:PhysicalEntity100001930 yago:WikicatJemezMountains yago:YagoGeoEntity yago:YagoLegalActorGeo yago:YagoPermanentlyLocatedEntity yago:Shape100027807 yago:Space113910384 yago:Vent109470550
rdfs:label	Jemez Lineament (en)
rdfs:comment	The Jemez Lineament is a chain of late Cenozoic volcanic fields, 800 kilometers (500 mi) long, reaching from the Springerville and White Mountains volcanic fields in East-Central Arizona to the Raton-Clayton volcanic field in Northeastern New Mexico. (en)
foaf:depiction
dcterms:subject	Volcanoes of New Mexico Volcanism of New Mexico Jemez Mountains
Wikipage page ID	16364958 (xsd:integer)
Wikipage revision ID	1064641059 (xsd:integer)
Link from a Wikipage to another Wikipage	dbr:Carbon_dioxide San Carlos volcanic field Mesa de Maya Alkaline magma series Earth's mantle Stratovolcano Colorado Plateau Grants, New Mexico Mount Taylor (New Mexico) Calc-alkaline magma series Caldera Zuni-Bandera volcanic field Fault (geology) Hotspot (geology) Mazatzal orogeny Volcanoes of New Mexico Cenozoic Basement (geology) Island arc Isotopes of lead Dip (geology) High Plains (United States) Jemez Mountains Rio Grande Rift Arizona Yavapai orogeny Volcanic field Red Hill volcanic field Stable isotope Springerville volcanic field Volcanism of New Mexico New Mexico Ocate volcanic field Raton-Clayton volcanic field Jemez Mountains dbr:Uranium Tholeiitic magma series Oceanic crust Pumice Mohorovičić discontinuity Perlite Yellowstone hot spot Epithermal Seismic imaging Ma (unit) Subduction zone
Link from a Wikipage to an external page
sameAs	Jemez Lineament Jemez Lineament Jemez Lineament Jemez Lineament
dbp:wikiPageUsesTemplate	dbt:Convert dbt:Coord_missing dbt:Reflist dbt:Short_description
thumbnail	wiki-commons:Special:FilePath/Jemez_Lineament.png?width=300
has abstract	The Jemez Lineament is a chain of late Cenozoic volcanic fields, 800 kilometers (500 mi) long, reaching from the Springerville and White Mountains volcanic fields in East-Central Arizona to the Raton-Clayton volcanic field in Northeastern New Mexico. The lineament was long interpreted as a hotspot trace (Raton hotspot) due to its resemblance in length and direction to the Yellowstone hot spot trace, but there is no systematic progression in age along the trace and it is now interpreted as a hydrous subduction zone scar. This formed about 1.7 billion years ago, when oceanic crust was subducting under what was then the southern edge of North America. The arrival of a large island arc in the subduction zone shifted subduction further south, leaving remnants of oceanic crust at the top of the Earth's mantle along the former subduction zone. These are rich in hydrous minerals that lower the melting temperature of the rock containing them. This hydrous subduction scar now separates basement rock of the Yavapai-Mazatzal transition zone from the Mazaztl Province proper. (en)
prov:wasDerivedFrom	wikipedia-en:Jemez_Lineament?oldid=1064641059&ns=0
page length (characters) of wiki page	9061 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Jemez_Lineament
is Link from a Wikipage to another Wikipage of	Caja del Rio Valles Caldera Geology of New Mexico Cima volcanic field El Malpais National Monument Mount Taylor (New Mexico) Basin and Range Province Zuni-Bandera volcanic field Mazatzal orogeny Taos Plateau volcanic field

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