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About: Taupo Bank     Goto   Sponge   NotDistinct   Permalink

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The Taupo Bank (also previously known as Mont Taupo,Taupo Guyot or Taupo Tablemount) is an extinct volcanic seamount of the Tasmantid Seamount Chain. It is a basaltic volcano that erupted between 10,300,000 to 11,400,000 years ago, with survey data that indicates it rises about 3,160 m (10,370 ft) above the local sea floor to a minimum depth of 128 m (420 ft). The sediments deposited on top of the alkali olivine basalt originate from the Late Miocene. It was likely a coral-capped volcanic seamount during the Pleistocene low sea level. It was described as a seamount in 1961.