An Entity of Type: Thing, from Named Graph: http://dbpedia.org, within Data Space: dbpedia.org

The Wyoming batholith is a granite batholith of Neoarchean origin 2,800 to 2,500 million years ago—which forms the eroded core of the Granite and Laramie Mountains in central Wyoming. The Wyoming batholith lies within the Wyoming Craton. The batholith, in its time, was a magma chamber. Contemporary magma chambers are filled with lava and buried deeply and are inaccessible. The Wyoming batholith is accessible for study, its overburden having eroded away.

Property Value
dbo:abstract
  • The Wyoming batholith is a granite batholith of Neoarchean origin 2,800 to 2,500 million years ago—which forms the eroded core of the Granite and Laramie Mountains in central Wyoming. The Wyoming batholith lies within the Wyoming Craton. The batholith, in its time, was a magma chamber. Contemporary magma chambers are filled with lava and buried deeply and are inaccessible. The Wyoming batholith is accessible for study, its overburden having eroded away. (en)
  • Il batolite del Wyoming è un batolite di composizione granitica la cui origine risale al Neoarcheano; il batolite si estende per oltre 200 km e forma il nucleo eroso delle Granite Mountains e delle Laramie Mountains, situate nella parte centrale dello stato del Wyoming, negli Stati Uniti d'America. Il batolite del Wyoming si trova all'interno del cratone del Wyoming e originariamente era una camera magmatica. Le camere magmatiche risalenti allo stesso periodo si trovano attualmente in profondità, sono riempite di lava e risultano inaccessibili. Nel caso del batolite del Wyoming, gli strati sovrastanti sono stati erosi nel corso del tempo, cosicché esso risulta esposto e accessibile allo studio. (it)
dbo:wikiPageID
  • 50761007 (xsd:integer)
dbo:wikiPageLength
  • 1820 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID
  • 843935211 (xsd:integer)
dbo:wikiPageWikiLink
dbp:wikiPageUsesTemplate
dcterms:subject
rdfs:comment
  • The Wyoming batholith is a granite batholith of Neoarchean origin 2,800 to 2,500 million years ago—which forms the eroded core of the Granite and Laramie Mountains in central Wyoming. The Wyoming batholith lies within the Wyoming Craton. The batholith, in its time, was a magma chamber. Contemporary magma chambers are filled with lava and buried deeply and are inaccessible. The Wyoming batholith is accessible for study, its overburden having eroded away. (en)
  • Il batolite del Wyoming è un batolite di composizione granitica la cui origine risale al Neoarcheano; il batolite si estende per oltre 200 km e forma il nucleo eroso delle Granite Mountains e delle Laramie Mountains, situate nella parte centrale dello stato del Wyoming, negli Stati Uniti d'America. (it)
rdfs:label
  • Batolite del Wyoming (it)
  • Wyoming batholith (en)
owl:sameAs
prov:wasDerivedFrom
foaf:isPrimaryTopicOf
is dbo:wikiPageWikiLink of
is foaf:primaryTopic of
Powered by OpenLink Virtuoso    This material is Open Knowledge     W3C Semantic Web Technology     This material is Open Knowledge    Valid XHTML + RDFa
This content was extracted from Wikipedia and is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License