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About: Phoenix Plate     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:Whole100003553, within Data Space : dbpedia.org associated with source document(s)

Type: anatomical structuregeo:SpatialThingyago:Artifact100021939yago:Base102797881yago:BaseballEquipment102799897yago:Equipment103294048yago:HomePlate103528901yago:Instrumentality103575240yago:Object100002684yago:PhysicalEntity100001930yago:WikicatHistoricalTectonicPlatesyago:SportsEquipment104285146yago:Whole100003553 New Facet based on Instances of this Class

The Phoenix Plate (also known as the Aluk Plate or Drake Plate) was a tectonic plate that existed during the early Paleozoic through late Cenozoic time. It formed a triple junction with the Izanagi and Farallon plates in the Panthalassa Ocean as early as 410 million years ago, during which time the Phoenix Plate was subducting under eastern Gondwana. During the Late Cretaceous or early Cenozoic, the southwestern part of the Phoenix Plate fragmented into the Charcot Plate, much in the same way in which the Rivera and Cocos plates were formed by the fragmentation of the Farallon Plate.