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About: Marysvale volcanic field     Goto   Sponge   NotDistinct   Permalink

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

Type: Thingplacedbo:Locationschema:Mountainschema:Placenatural placeMountainyago:WikicatMioceneVolcanoesyago:WikicatVolcanicFieldsOfTheGreatBasinSectionyago:WikicatVolcanoesOfUtahgeo:SpatialThingyago:WikicatOligoceneVolcanoesyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:Field108569998yago:GeographicalArea108574314yago:GeologicalFormation109287968yago:Location100027167yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:Region108630985yago:WikicatHoloceneVolcanoesyago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntitymountainyago:Shape100027807yago:Space113910384yago:Tract108673395yago:Vent109470550yago:WikicatPleistoceneVolcanoesyago:WikicatPlioceneVolcanoes New Facet based on Instances of this Class

The Marysvale volcanic field is located in southwestern Utah, United States. One of the largest volcanic fields in the western United States, the Marysvale straddles the Colorado Plateau-Great Basin transition zone. Most igneous rocks belong to a middle Cenozoic (~32 to 22 million years old) calc-alkaline sequence, although about 5% are related to an upper Cenozoic (23 million years to Holocene) bimodal (basalt and rhyolite) sequence. The Marysvale contains a variety of volcanic features, including stratovolcanoes, calderas, lava domes, and cinder cones.