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About: Kawdy Mountain     Goto   Sponge   NotDistinct   Permalink

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

Type: Thingplacedbo:Locationschema:Mountainschema:Placenatural placeMountainyago:WikicatMonogeneticVolcanoesyago:WikicatMountainsOfBritishColumbiayago:WikicatVolcanoesOfBritishColumbiageo:SpatialThingyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:GeologicalFormation109287968yago:Location100027167yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntityhistoric placemountainyago:Shape100027807yago:Space113910384yago:Vent109470550yago:WikicatPleistoceneVolcanoesumbel-rc:Mountain New Facet based on Instances of this Class

Kawdy Mountain is a subglacial mound on the Kawdy Plateau, the northernmost sub-plateau of the Stikine Plateau in northwestern British Columbia, Canada. It consists of nearly horizontal beds of basaltic lava, capping outward dipping beds of fragmental volcanic rocks and last erupted in Pleistocene. Kawdy Mountain is one of many basaltic volcanic features of the Stikine Volcanic Belt, which is forming because the North American tectonic plate is stretching slightly as it moves to the west.