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  2. Lake Taupō - Wikipedia

    en.wikipedia.org/wiki/Lake_Taupō

    Lake Taupō has a perimeter of approximately 193 km (120 mi) and a maximum depth of 186 m (610 ft). It is drained by the Waikato River (New Zealand's longest river), and its main tributaries are the Waitahanui River, the Tongariro River, and the Tauranga Taupō River. It is a noted trout fishery with stocks of introduced brown and rainbow trout.

  3. Taupō Volcano - Wikipedia

    en.wikipedia.org/wiki/Taupō_Volcano

    Lake Taupō, in the centre of New Zealand's North Island, fills the caldera of the Taupō Volcano, a large rhyolitic supervolcano.This huge volcano has produced two of the world's most powerful eruptions in geologically recent times.

  4. Taupō - Wikipedia

    en.wikipedia.org/wiki/Taupō

    Taupō (Māori pronunciation: [ˈ t a ʉ p ɔː]), sometimes written Taupo, is a town located in the central North Island of New Zealand. It is situated on the edge of Lake Taupō , which is the largest freshwater lake in New Zealand.

  5. List of lakes of New Zealand - Wikipedia

    en.wikipedia.org/wiki/List_of_lakes_of_New_Zealand

    Lake Taupō, New Zealand's largest lake Lake Wakatipu from Queenstown Lake Tekapo Lake Rotorua from above Rotorua Lake Hauroko, New Zealand's deepest lake Ōkārito Lagoon. This is a list of lakes in New Zealand. A lake's location is identified by the region and either the territorial authority or national park (N.P.). There are:

  6. Hatepe eruption - Wikipedia

    en.wikipedia.org/wiki/Hatepe_eruption

    The Hatepe eruption, named for the Hatepe Plinian pumice tephra layer, [1] sometimes referred to as the Taupō eruption or Horomatangi Reef Unit Y eruption, is dated to 232 CE ± 10 [2] and was Taupō Volcano's most recent major eruption. It is thought to be New Zealand's largest eruption within the last

  7. Oruanui eruption - Wikipedia

    en.wikipedia.org/wiki/Oruanui_eruption

    The former Lake Huka that had extended to the north and partially occupied the older Reporoa Caldera was destroyed and filled in with ignimbrite, which also created a temporary barrier between the Taupō and Reporoa watersheds that had to be eroded before a stable drainage of the new Lake Taupō was established.