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About: East Tasman Plateau     Goto   Sponge   NotDistinct   Permalink

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

Type: yago:WikicatUnderwaterRidgesOfThePacificOceangeo:SpatialThingyago:GeologicalFormation109287968yago:Highland109302616yago:NaturalElevation109366317yago:Object100002684yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntityyago:Ridge109409512yago:Tableland109453008yago:WikicatPlateausOfThePacificOcean New Facet based on Instances of this Class

The East Tasman Plateau is a submerged microcontinent south east of Tasmania. Its area is 50,000 square kilometres (19,000 sq mi), and it is mostly from 2,500 to 3,000 metres (8,200 to 9,800 ft) deep. It is a circular piece of continental rocks surrounded by oceanic crust. Volcanism occurred there 36 million years ago. The East Tasman Plateau is separated from the island of Tasmania by 100 kilometres (62 mi) of deeper water, and the East Tasman Saddle is a higher ridge connecting the plateau to the Freycinet Peninsula region of the Tasmanian East Coast. This ridge runs north west from the plateau. South-west of the plateau is the . The East Tasman Plateau represents a continental fragment.