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Statements

Subject Item
dbr:Trans-Pecos_Volcanic_Field
rdf:type
geo:SpatialThing
rdfs:label
Trans-Pecos Volcanic Field
rdfs:comment
The Trans-Pecos Volcanic Field is a volcanic field located in western Texas in the counties of Brewster, Jeff Davis, Presidio, and extends into northern Mexican states of Chihuahua and Coahuila. It is the southernmost volcanic field to be documented and recorded in the continental United States. The field started volcanic activity around 48 million years ago in the middle Eocene epoch, and ended around 17 million years later in the Miocene epoch. The Volcanic field is the result of Ancient Subduction off the western portion of the continent at the time.
geo:lat
29.22500038146973
geo:long
-103.4990005493164
dcterms:subject
dbc:Eocene_volcanism dbc:Volcanism_of_Mexico dbc:Miocene_volcanism dbc:Volcanic_fields_of_the_United_States dbc:Oligocene_volcanism
dbo:wikiPageID
65730449
dbo:wikiPageRevisionID
1107596126
dbo:wikiPageWikiLink
dbr:Jeff_Davis_County,_Texas dbr:Chinati_Mountain_Caldera_Complex dbr:Solitario dbc:Miocene_volcanism dbr:Miocene dbc:Volcanism_of_Mexico dbr:Pine_Canyon_caldera_complex dbc:Volcanic_fields_of_the_United_States dbr:Christmas_Mountains_caldera_complex dbr:Chihuahua_(state) dbr:Subduction dbr:Big_Bend_National_Park dbr:Big_Bend_Ranch_State_Park dbr:Continental_United_States dbr:Alpine,_Texas dbr:Volcanic_field dbr:Presidio_County dbr:Caldera dbr:Texas dbr:United_States_Geological_Survey dbr:Coahuila dbr:Presidio_County,_Texas dbc:Oligocene_volcanism dbr:Brewster_County,_Texas dbr:Paisano_Volcano dbr:Mexico dbr:Davis_Mountains_Caldera_Complex dbr:Bofecitos_mountains_center dbr:Eocene dbc:Eocene_volcanism
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n9:FU7Jp wikidata:Q104867385
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georss:point
29.225 -103.499
dbo:abstract
The Trans-Pecos Volcanic Field is a volcanic field located in western Texas in the counties of Brewster, Jeff Davis, Presidio, and extends into northern Mexican states of Chihuahua and Coahuila. It is the southernmost volcanic field to be documented and recorded in the continental United States. The field started volcanic activity around 48 million years ago in the middle Eocene epoch, and ended around 17 million years later in the Miocene epoch. The Volcanic field is the result of Ancient Subduction off the western portion of the continent at the time. Most of the volcanoes in the field are calderas. Some of the volcanoes are: * In Big Bend National Park, the Christmas Mountains caldera complex and Pine Canyon caldera complex * In Big Bend Ranch State Park, the and the Solitario * Near Alpine, the * In northern Jeff Davis County, the * In central Presidio County, the Chinati Mountain Caldera Complex, and the Oak Hills Center. The field is currently undergoing geological studying and researched by several colleges and the United States Geological Survey.
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wikipedia-en:Trans-Pecos_Volcanic_Field?oldid=1107596126&ns=0
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2574
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wikipedia-en:Trans-Pecos_Volcanic_Field
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POINT(-103.49900054932 29.22500038147)