Haroharo Caldera

The Haroharo Caldera (Haroharo volcanic complex) is a 26 by 16 km (16.2 by 9.9 mi) postulated volcanic feature in Taupō Volcanic Zone of the North Island, New Zealand within the larger and older Ōkataina Caldera. Since 2010 further studies have tended to use the terms Haroharo vent alignment, Utu Caldera, Matahina Caldera, Rotoiti Caldera and a postulated Kawerau Caldera to the features assigned to it.[1] However the name is used in the peer reviewed literature to summarise and group these features based on gravitational and magnetic features.[2]: 14 

Main article: Ōkataina Caldera
  1. ^ Hughes, Ery C.; Law, Sally; Kilgour, Geoff; Blundy, Jon D.; Mader, Heidy M. (2023). "Storage, evolution, and mixing in basaltic eruptions from around the Okataina Volcanic Centre, Taupō Volcanic Zone, Aotearoa New Zealand". Journal of Volcanology and Geothermal Research. 434 (107715). doi:10.1016/j.jvolgeores.2022.107715. hdl:20.500.11820/9f5c151c-1f2e-47ed-a264-7649eacdf669. ISSN 0377-0273. S2CID 253783414.
  2. ^ Caratori Tontini, F; de Ronde, CEJ; Black, J; Stucker, VK; Walker, SL (2023). "The geology and geophysics of Lake Tarawera, New Zealand: Implications for sublacustrine geothermal activity". Journal of Volcanology and Geothermal Research. 433. doi:10.1016/j.jvolgeores.2022.107731. ISSN 0377-0273.