Pinos volcanic complex (original) (raw)
The Pinos volcanic complex is an extinct volcanic complex in the Pinos Municipality, Zacatecas and Ahualulco Municipality in San Luis Potosí, Mexico, which was active during the Middle Tertiary, it was discovered due to having been found volcanic rocks, sedimentary rocks, conglomerate sandstone, red beds 900 meters thick, inhomogeneous mixture of magma, polymitic and granite with muscovite and tourmaline. The complex is mainly composed of lava domes, volcanic tuffs and geological faults, the period of activity was between about 32 ma–27 ma.
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| dbo:abstract | The Pinos volcanic complex is an extinct volcanic complex in the Pinos Municipality, Zacatecas and Ahualulco Municipality in San Luis Potosí, Mexico, which was active during the Middle Tertiary, it was discovered due to having been found volcanic rocks, sedimentary rocks, conglomerate sandstone, red beds 900 meters thick, inhomogeneous mixture of magma, polymitic and granite with muscovite and tourmaline. The complex is mainly composed of lava domes, volcanic tuffs and geological faults, the period of activity was between about 32 ma–27 ma. (en) |
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| dbo:wikiPageRevisionID | 1108551340 (xsd:integer) |
| dbo:wikiPageWikiLink | dbr:San_Luis_Potosí dbr:Red_beds dbc:Volcanoes_of_Zacatecas dbr:Conglomerate_(geology) dbr:Zacatecas dbc:Complex_volcanoes dbr:Volcanic_complex dbr:Extinct_volcano dbr:Tertiary dbr:Pinos_Municipality dbr:Mexico dbc:Oligocene_volcanoes dbr:Sedimentary_rocks dbr:Mega-annum dbr:Volcanic_rocks dbr:Ahualulco_Municipality dbr:Volcanic_tuff dbr:Lava_domes |
| dbp:wikiPageUsesTemplate | dbt:Coord dbt:Reflist dbt:Volcanology-stub dbt:Zacatecas-geo-stub |
| dcterms:subject | dbc:Volcanoes_of_Zacatecas dbc:Complex_volcanoes dbc:Oligocene_volcanoes |
| georss:point | 22.340053 -101.501023 |
| rdf:type | geo:SpatialThing |
| rdfs:comment | The Pinos volcanic complex is an extinct volcanic complex in the Pinos Municipality, Zacatecas and Ahualulco Municipality in San Luis Potosí, Mexico, which was active during the Middle Tertiary, it was discovered due to having been found volcanic rocks, sedimentary rocks, conglomerate sandstone, red beds 900 meters thick, inhomogeneous mixture of magma, polymitic and granite with muscovite and tourmaline. The complex is mainly composed of lava domes, volcanic tuffs and geological faults, the period of activity was between about 32 ma–27 ma. (en) |
| rdfs:label | Pinos volcanic complex (en) |
| owl:sameAs | wikidata:Pinos volcanic complex https://global.dbpedia.org/id/Gc7VQ |
| geo:geometry | POINT(-101.50102233887 22.34005355835) |
| geo:lat | 22.340054 (xsd:float) |
| geo:long | -101.501022 (xsd:float) |
| prov:wasDerivedFrom | wikipedia-en:Pinos_volcanic_complex?oldid=1108551340&ns=0 |
| foaf:isPrimaryTopicOf | wikipedia-en:Pinos_volcanic_complex |
| is dbo:wikiPageDisambiguates of | dbr:Pinos_(disambiguation) |
| is dbo:wikiPageWikiLink of | dbr:Pinos_(disambiguation) |
| is foaf:primaryTopic of | wikipedia-en:Pinos_volcanic_complex |