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About: Rabbit Mountain     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:Vent109470550, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: Thingplacedbo:Locationschema:Mountainschema:Placenatural placeMountainyago:WikicatVolcanoesOfYukongeo:SpatialThingyago:WikicatSubductionVolcanoesyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:GeologicalFormation109287968yago:Location100027167yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntitymountainyago:Shape100027807yago:Space113910384yago:Vent109470550 New Facet based on Instances of this Class

Rabbit Mountain is an eroded volcanic outcrop in the Wrangell Volcanic Field, Yukon Territory, Canada, located 30 km southwest of and 4 km northwest of . It is east of the Yukon-Alaska boundary and can be accessed by old mining roads that reach Rabbit Creek. Rabbit Mountain formed as a result of melting of the crust, due to subduction of the Pacific Plate beneath the North American Plate and last erupted during the Pliocene. Like most volcanoes in the Yukon, Rabbit Mountain is part of the Pacific Ring of Fire, that includes over 160 active volcanoes.