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About: 2012 Kermadec Islands eruption     Goto   Sponge   NotDistinct   Permalink

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

Type: yago:WikicatVolcanoesOfNewZealandgeo:SpatialThingyago:WikicatSeamountsOfThePacificOceanyago:WikicatSubmarineVolcanoesyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:GeologicalFormation109287968yago:Island109316454yago:Land109334396yago:Location100027167yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:WikicatKermadecIslandsyago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntitydiseaseyago:Seamount109427752yago:Shape100027807yago:Space113910384yago:Vent109470550yago:WikicatActiveVolcanoesyago:WikicatFloatingIslands New Facet based on Instances of this Class

The 2012 Kermadec Islands eruption was a major undersea volcanic eruption that was produced by the previously little-known Havre Seamount near the L'Esperance and L'Havre Rocks in the Kermadec Islands of New Zealand. The large volume of low density pumice produced by the eruption accumulated as a large area of floating pumice, a pumice raft, that was originally covering a surface of 400 square kilometres (150 square miles), spread to a continuous float of between 19,000 and 26,000 square kilometres (7,500 and 10,000 sq mi) and within three months dispersed to an area of more than twice the size of New Zealand.