About: Pabellón de Inca

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

Pabellón de Inca is a volcano in Chile. Located in the Tarapacá Region, it rises 1,000 metres (3,300 ft) above the basement. Volcanic activity in the region during the Eocene had formed the Icanche Formation, about 45 million years ago. After a pause of about 33 million years, volcanic activity resumed during the Miocene and continues to the present day. The volcanism included the Uijna and Carcote ignimbrites and the stratovolcanoes on the border between Chile and Bolivia. Pabellón de Inca, Irruputuncu and Poruñita have erupted andesite and dacite. They contain hornblende and pyroxene.

Property Value
dbo:abstract
  • Pabellón de Inca is a volcano in Chile. Located in the Tarapacá Region, it rises 1,000 metres (3,300 ft) above the basement. Volcanic activity in the region during the Eocene had formed the Icanche Formation, about 45 million years ago. After a pause of about 33 million years, volcanic activity resumed during the Miocene and continues to the present day. The volcanism included the Uijna and Carcote ignimbrites and the stratovolcanoes on the border between Chile and Bolivia. Together with Irruputuncu and del Inca and Poruñita it is considered to be a young volcano. Lava flows and craters are no longer recognizable but the volcano maintains a conical shape. Other volcanoes in the area are El Rojo Sur and Olca-Paruma. Pabellón de Inca is not active. Pabellón de Inca, Irruputuncu and Poruñita have erupted andesite and dacite. They contain hornblende and pyroxene. The tree Polylepis tarapacana is found on Pabellón de Inca. (en)
dbo:wikiPageExternalLink
dbo:wikiPageID
  • 53857957 (xsd:integer)
dbo:wikiPageLength
  • 3696 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID
  • 1116061596 (xsd:integer)
dbo:wikiPageWikiLink
dbp:wikiPageUsesTemplate
dcterms:subject
georss:point
  • -20.916666666666668 -68.61666666666666
rdf:type
rdfs:comment
  • Pabellón de Inca is a volcano in Chile. Located in the Tarapacá Region, it rises 1,000 metres (3,300 ft) above the basement. Volcanic activity in the region during the Eocene had formed the Icanche Formation, about 45 million years ago. After a pause of about 33 million years, volcanic activity resumed during the Miocene and continues to the present day. The volcanism included the Uijna and Carcote ignimbrites and the stratovolcanoes on the border between Chile and Bolivia. Pabellón de Inca, Irruputuncu and Poruñita have erupted andesite and dacite. They contain hornblende and pyroxene. (en)
rdfs:label
  • Pabellón de Inca (en)
owl:sameAs
geo:geometry
  • POINT(-68.616668701172 -20.916666030884)
geo:lat
  • -20.916666 (xsd:float)
geo:long
  • -68.616669 (xsd:float)
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