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About: Rano Kau     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatPleistoceneVolcanoes, within Data Space : dbpedia.org associated with source document(s)

Type: Thingyago:WikicatArchaeologicalSitesInChileyago:WikicatCraterLakesyago:WikicatMountainsOfChileyago:WikicatVolcanicCalderasOfChileyago:WikicatVolcanicCratersyago:WikicatVolcanoesOfChileyago:WikicatVolcanoesOfEasterIslandyago:WikicatVolcanoesOfThePacificOceanyago:WikicatWorldHeritageSitesInChilegeo:SpatialThingyago:WikicatShieldVolcanoesyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:BodyOfWater109225146yago:Caldera109231117yago:Crack109258715yago:GeographicalArea108574314yago:GeologicalFormation109287968yago:Lake109328904yago:Location100027167yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:Region108630985yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntityyago:Shape100027807yago:Site108651247yago:Space113910384yago:Thing100002452yago:Tract108673395yago:Vent109470550yago:VolcanicCrater109472413yago:WikicatExtinctVolcanoesyago:WikicatPleistoceneVolcanoes New Facet based on Instances of this Class

Rano Kau is a 324 m (1,063 ft) tall dormant volcano that forms the southwestern headland of Easter Island, a Chilean island in the Pacific Ocean. It was formed of basaltic lava flows in the Pleistocene with its youngest rocks dated at between 150,000 and 210,000 years ago.