Pocho volcanic field
http://dbpedia.org/resource/Pocho_volcanic_field an entity of type: SpatialThing
Los volcanes de Pocho son conjunto de diez conos volcánicos en el extremo sur de Sierras de Guasapampa en Valle de Traslasierra que se consideran extinguidos, siendo conocidos sus principales picos:
* La Ciénaga o Boroa (1.300 m.s.n.m.)
* Poca (1.600 m.s.n.m.),
* Yerba Buena (1.760 m.s.n.m.) Se ubican a 140 kilómetros al oeste de la ciudad de Córdoba, y próximos a las localidades de Taninga y Salsacate, en el departamento Pocho. Se accede a ellos mediante la ruta provincial 28, que une estas dos localidades con provincia de La Rioja.
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Pocho volcanic field is a volcanic field in Argentina. It is associated with a crustal lineament known as the Ojo de Agua Lineament. It is located in the Sierras de Cordoba mountain chain. It formed during the late Miocene, when a progressive shallowing of the subducting Nazca Plate caused volcanic activity to retreat 500 kilometres (310 mi) from the main Andes into the land behind the mountain chain. This did result in a typical shallow slab chemistry of the Pocho rocks. Volcanic activity at Pocho is dated about 4.7 +- 0.3 million years ago and took place over two cycles. Seismic activity in the area may indicate the presence of a residual magma chamber however, which would also explain anomalous crustal seismic velocities in the area.
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Volcanes de Pocho
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Pocho volcanic field
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rdf:langString
Los volcanes de Pocho son conjunto de diez conos volcánicos en el extremo sur de Sierras de Guasapampa en Valle de Traslasierra que se consideran extinguidos, siendo conocidos sus principales picos:
* La Ciénaga o Boroa (1.300 m.s.n.m.)
* Poca (1.600 m.s.n.m.),
* Yerba Buena (1.760 m.s.n.m.) Se ubican a 140 kilómetros al oeste de la ciudad de Córdoba, y próximos a las localidades de Taninga y Salsacate, en el departamento Pocho. Se accede a ellos mediante la ruta provincial 28, que une estas dos localidades con provincia de La Rioja.
rdf:langString
Pocho volcanic field is a volcanic field in Argentina. It is associated with a crustal lineament known as the Ojo de Agua Lineament. It is located in the Sierras de Cordoba mountain chain. It formed during the late Miocene, when a progressive shallowing of the subducting Nazca Plate caused volcanic activity to retreat 500 kilometres (310 mi) from the main Andes into the land behind the mountain chain. This did result in a typical shallow slab chemistry of the Pocho rocks. Volcanic activity at Pocho is dated about 4.7 +- 0.3 million years ago and took place over two cycles. Seismic activity in the area may indicate the presence of a residual magma chamber however, which would also explain anomalous crustal seismic velocities in the area.
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