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About: Cerro El Cóndor     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatPolygeneticVolcanoes, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: Thingplacedbo:Locationschema:Placenatural placeVolcanovolcanoyago:WikicatMountainsOfArgentinayago:WikicatVolcanoesOfArgentinageo:SpatialThingyago:WikicatSubductionVolcanoesyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:GeologicalFormation109287968yago:Location100027167yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntityyago:Shape100027807yago:Space113910384yago:Vent109470550yago:WikicatPolygeneticVolcanoes New Facet based on Instances of this Class

Cerro El Cóndor is a stratovolcano in Argentina. Cerro El Cóndor is a remote peak in the Argentine Puna de Atacama. As such it was probably the last major 6000m+ peak in the Andes to be climbed, with the summit reaching a height of 6,400 metres (21,000 ft). The volcano has the form of a massif (which covers a surface of 281 square kilometres (108 sq mi)) constructed by two separate volcanoes; the older edifice forms parts of the northern and eastern flanks which are cut by scarps interpreted as caldera remnants. The summit region is formed by the newer edifice, and features a series of craters with diameters of 100–350 metres (330–1,150 ft) and a cover of pyroclastic material and scoria. Also part of the newer phase are extensive lava flows which form the western and parts of the eastern a