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About: Caloosahatchee Seamount     Goto   Sponge   NotDistinct   Permalink

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

Type: geo:SpatialThingyago:WikicatSeamountsOfTheAtlanticOceanyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:GeologicalFormation109287968yago:Location100027167yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:WikicatHotspotVolcanoesyago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntityyago:Seamount109427752yago:Shape100027807yago:Space113910384yago:Vent109470550 New Facet based on Instances of this Class

The Caloosahatchee Seamount is a seamount in the northern Atlantic Ocean. It is part of the Corner Rise Seamounts, which was active about 75 million years ago. It was formed when the North American Plate moved over the New England hotspot, also known as the Great Meteor Hotspot. The Great Meteor Hotspot also formed various kimberlite fields in Canada, the Monteregian Hills, the White Mountains, the New England Seamounts, and the Seewarte Seamounts, which are the newest volcanoes produced by the New England Hotspot.