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About: Mono–Inyo Craters     Goto   Sponge   NotDistinct   Permalink

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

Type: Thingcompanyplacedbo:Locationschema:Mountainschema:Placenatural placeMountainyago:WikicatVolcanicFieldsOfTheGreatBasinSectionyago:WikicatVolcanoesOfCaliforniayago:WikicatVolcanoesOfMonoCounty,Californiageo:SpatialThingyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:Field108569998yago:GeographicalArea108574314yago:GeologicalFormation109287968yago:Location100027167yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:Range109403734yago:Region108630985yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntitymountainyago:Shape100027807yago:Space113910384yago:Tract108673395yago:Vent109470550 New Facet based on Instances of this Class

The Mono–Inyo Craters are a volcanic chain of craters, domes and lava flows in Mono County, Eastern California. The chain stretches 25 miles (40 km) from the northwest shore of Mono Lake to the south of Mammoth Mountain. The Mono Lake Volcanic Field forms the northernmost part of the chain and consists of two volcanic islands in the lake and one cinder cone volcano on its northwest shore. Most of the Mono Craters, which make up the bulk of the northern part of the Mono–Inyo chain, are phreatic (steam explosion) volcanoes that have since been either plugged or over-topped by rhyolite domes and lava flows. The Inyo volcanic chain form much of the southern part of the chain and consist of phreatic explosion pits, and rhyolitic lava flows and domes. The southernmost part of the chain consists