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  2. Taupō Volcano - Wikipedia

    en.wikipedia.org/wiki/Taupō_Volcano

    The eruption further expanded the lake, which had formed after the much larger Oruanui eruption. Its new deposits also briefly created another large lake to the Taupō Volcano's north that extended to the Reporoa Caldera which in due course broke out into the Waikato River valley and released over a short period 2.5 km 3 (0.60 cu mi) of water.

  3. Oruanui eruption - Wikipedia

    en.wikipedia.org/wiki/Oruanui_eruption

    At the time of the eruption, the sea level was much lower than at present, and for over 100,000 years the Taupō Volcano had been mainly under Lake Huka, a larger lake than the present Lake Taupō. [1]: 6 Lake Huka was destroyed in the eruption, and other features of the local geography were changed significantly as outlined below.

  4. Lake Taupō - Wikipedia

    en.wikipedia.org/wiki/Lake_Taupō

    Lake Taupō (also spelled Taupo; Māori: Taupō-nui-a-Tia or Taupōmoana) is a large crater lake in New Zealand's North Island, located in the caldera of Taupō Volcano. The lake is the namesake of the town of Taupō , which sits on a bay in the lake's northeastern shore.

  5. Hatepe eruption - Wikipedia

    en.wikipedia.org/wiki/Hatepe_eruption

    In due course after the Hatepe eruption the lake that formed further expanded on the lake that had formed after the much larger Oruanui eruption around 26,500 years ago. The previous outlet was blocked, raising the lake 35 meters (115 feet) above its present level until it broke out after about 20 years in a huge flood. [6]

  6. Mount Tauhara - Wikipedia

    en.wikipedia.org/wiki/Mount_Tauhara

    Mount Tauhara is a dormant lava dome [1] volcano in New Zealand's North Island, reaching 1,088 metres (3,570 ft) above sea level.It is situated in the area of caldera rim overlap of the Whakamaru Caldera and Taupō Volcano towards the centre of the Taupō Volcanic Zone, which stretches from Whakaari / White Island in the north to Mount Ruapehu in the south. [2]

  7. Horomatangi Reef - Wikipedia

    en.wikipedia.org/wiki/Horomatangi_Reef

    The reefs are at a high heat-output geothermal hot spot area within the Taupō Volcano. [3] This is related to rhyolitic lava domes extruded after explosive volcanism. [4] The explosive eruptions include the VEI 7 Hatepe eruption of 232 ± 10 CE that ejected over 120 km 3 (29 cu mi) of material (also known as Horomatangi Reef Unit Y eruption) [5] and its linear line of eruption centres, [6] as ...

  8. Video shows volcanic eruption in Indonesia, not Yellowstone ...

    www.aol.com/video-shows-volcanic-eruption...

    The video shows August footage from Mount Dukono, an active volcano in Indonesia, not Yellowstone National Park. No evidence supports the post’s claim of a Yellowstone volcanic eruption in ...

  9. Taupō Volcanic Zone - Wikipedia

    en.wikipedia.org/wiki/Taupō_Volcanic_Zone

    The other volcanic plateau defining eruptions were to the west, the 150 km 3 (36 cu mi) Matahina eruption of about 280,000 years ago, the mainly tephra 50 km 3 (12 cu mi) Chimp (Chimpanzee) eruption between 320 and 275 ka, the central 50 km 3 (12 cu mi) Pokai eruption of about 275 ka, and the paired Mamaku to the north and east central Ohakuri ...