Kōrero: Volcanoes

Lake Taupō

Lake Taupō

Lake Taupō occupies a caldera (collapse crater), formed by the Ōruanui eruption, and modified by later eruptions. Using information from a survey of the lake, this image shows the shape and depth of the lake bed. The deepest part is near Horomatangi Reefs, where there are hydrothermal vents on the lake floor.

Te whakamahi i tēnei tūemi

NIWA – National Institute of Water and Atmospheric Research

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Ngā whakaahua me ngā rauemi katoa o tēnei kōrero

Te tuhi tohutoro mō tēnei whārangi:

Richard Smith, David J. Lowe and Ian Wright, 'Volcanoes - The Taupō volcano', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/mi/diagram/8712/lake-taupo (accessed 18 November 2019)

He kōrero nā Richard Smith, David J. Lowe and Ian Wright, i tāngia i te 12 Jun 2006