taupo volcanic zone

Mount Tarawera is a volcano on the North Island of New Zealand. All lie within the Okataina caldera, along its western edge. [3], The last major eruption from Lake Taupo, the Hatepe eruption, occurred in 232 AD. Eerder werd aangenomen dat de datum van deze activiteit 186 na Christus was, aangezien men dacht dat de asuitstoot groot genoeg was om de hemel rood te kleuren boven Rome en China (zoals gedocumenteerd in Hou Han Shu ), maar dit is sindsdien weerlegd. Taupo, the most active rhyolitic volcano of the Taupo volcanic zone, is a large, roughly 35-km-wide caldera with poorly defined margins. De vulkanische zone Taupo is ongeveer 350 kilometer (217 mijl) lang en 50 kilometer (31 mijl) breed. There is nowadays a somewhat different classification: [18] [19]. The date of this activity was previously thought to be 186AD as the ash expulsion was thought to be sufficiently large to turn the sky red over Rome and China (as documented in Hou Han Shu), but this has since been disproven. [5], It forms a southern portion of the active Lau-Havre-Taupo back-arc basin, which lies behind the Kermadec-Tonga subduction zone. The Taupo Volcanic Zone is named after Lake Taupo, the largest volcano in the zone. You would need more than 20,000 of these to fill just one cubic kilometre. Lake Tarawera is the largest of a series of lakes which surround the volcano Mount Tarawera in the North Island of New Zealand. Hoewel het back-arc-bassin zich naar het zuidwesten blijft voortplanten, waarbij het South Wanganui-bassin een aanvankelijk back-arc-bassin vormt, is er in deze regio nog geen vulkanische activiteit begonnen. Other important features of the TVZ include the Whakatane, Ngakuru and Ruapehu grabens. The region around the city of Rotorua, in New Zealand's North Island, contains several lakes. We also see fumaroles, mud pools and of course hydrothermal eruptions including geysers of which Orakei Korako has the most of any site in New Zealand. In football, you use your speed for e.g; This process has been going on since before the Hatepe eruption. Ten oosten van de belangrijkste breukzone: Reporoa enkele gebeurtenis caldera; Kaingaroa Ignimbrite (circa 240.000 jaar oud), Zuidelijk deel: Tongariro vulkanisch centrum, Deze pagina is voor het laatst bewerkt op 10 oktober 2020 om 03:56, This page is based on the copyrighted Wikipedia article. Mount Ruapehu marks its south-western end and the zone runs north-eastward through the Taupo and Rotorua areas and offshore into the Bay of Plenty. There is also some possible rifting in the Taupo Volcanic Zone.

There is nowadays a somewhat different classification:[19][20], List of volcanoes in New Zealand § Taupo Volcanic Zone, "Hf isotope evidence for variable slab input and crustal addition in basalts and andesites of the Taupo Volcanic Zone, New Zealand", "Polynesian settlement and impacts of volcanism on early Maori society", "Seafloor geology and petrology in the oceanic to continental transition zone of the Kermadec-Havre-Taupo Volcanic Zone arc system, New Zealand", "Early evolution of a young back-arc basin in the Havre Trough", "Evolution of the southern termination of the Taupo Rift, New Zealand", "Central North Island sitting on magma film", "Imaging magmatic Processes in the Taupo Volcanic Zone (New Zealand) with Magnetotellurics", http://www.volcano.si.edu/world/largeeruptions.cfm, "Historical unrest at large calderas of the world", "The Sedimentation and Drainage History of Haroharo Caldera and The Tarawera River System, Taupo Volcanic Zone, New Zealand", "Petrography and geochemistry of lithic fragments in ignimbrites from the Mangakino Volcanic Centre: implications for the composition of the subvolcanic crust in western Taupo Volcanic Zone, New Zealand", "Caldera volcanism and rift structure in the Taupo Volcanic Zone, New Zealand", "The nature and age of Ohakuri Formation and Ohakuri Group rocks in surface exposures and geothermal drillhole sequences in the central Taupo Volcanic Zone, New Zealand", New Zealand's volcanoes: The Taupo Volcanic Centre, New Zealand's volcanoes: The Okataina Volcanic Centre, Environment Bay of Plenty, Regional Council, Library, Environment Waikato, Regional Council, map, Geological Society of New Zealand & New Zealand Geophysical Society - Fieldtrip 2, New Zealand, Taupo and Coromandel volcanic zones, The Taupo Volcanic Zone with Māori Freehold Land (1995) - showing geothermal fields, https://en.wikipedia.org/w/index.php?title=Taupo_Volcanic_Zone&oldid=982754780, Creative Commons Attribution-ShareAlike License, Okataina Caldera, size: roughly 27 x 20 km, Haroharo volcanic complex, northern end of the Okataina Volcanic Center, North part: Whakatane Graben – Bay of Plenty, Mangakino caldera complex; may be transitional between Coromandel Volcanic Zone (CVZ) and Taupo Volcanic Zone (TVZ) (1.62 – 0.91 mio.

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