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About: Ice Peak     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : umbel-rc:Mountain, within Data Space : dbpedia.org associated with source document(s)

Type: Thingplacedbo:Locationschema:Placenatural placeVolcanovolcanoyago:WikicatMountainsOfBritishColumbiayago:WikicatVolcanicCalderasOfCanadayago:WikicatVolcanoesOfBritishColumbiageo:SpatialThingyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Caldera109231117yago:Crack109258715yago:GeologicalFormation109287968yago:Location100027167yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntityyago:Shape100027807yago:Space113910384yago:Vent109470550yago:VolcanicCrater109472413yago:WikicatPleistoceneVolcanoesyago:WikicatPolygeneticVolcanoesumbel-rc:Mountain New Facet based on Instances of this Class

Ice Peak is a stratovolcano, located 39 km (24 mi) west of Tatogga and 3 km (2 mi) south of Mount Edziza, British Columbia, Canada. It overlaps the 7.5-million-year-old Armadillo Peak. It lies on a large volcanic plateau, which is made of basaltic lava flows from the massive Mount Edziza volcanic complex. Ice Peak last erupted during the Holocene. The summit of Ice Peak is a remnant of the western rim of a small summit caldera, which has been nearly destroyed by alpine glaciation. Ice Peak gets name because it is almost completely surrounded by glaciers.