New Zealand · Caldera
Taupō Volcano
Taupo
- Type
- Caldera
- Elevation
- 760m
- Last eruption
- 260

- Type
- Caldera
- Country
- New Zealand
- Region
- Tonga & Kermadec / Taupo Volcanic Arc
- Elevation
- 760m
- Coordinates
- -38.781, 175.893
- Last eruption
- 260
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Caldera
- Major rock type
- Rhyolite
Geological summary
Taupo, the most active rhyolitic volcano of the Taupo volcanic zone, is a large, roughly 35-km-wide caldera with poorly defined margins. It is a type example of an "inverse volcano" that slopes inward towards the most recent vent location. The caldera, now filled by Lake Taupo, largely formed as a result of the voluminous eruption of the Oruanui Tephra about 22,600 years before present (BP). This was the largest known eruption at Taupo, producing about 1,170 km3 of tephra. This eruption was preceded during the late Pleistocene by the eruption of a large number of rhyolitic lava domes north of Lake Taupo. Large explosive eruptions have occurred frequently during the Holocene from many vents within Lake Taupo and near its margins. The most recent major eruption took place about 1,800 years BP from at least three vents along a NE-SW-trending fissure centered on the Horomotangi Reefs. This extremely violent eruption was New Zealand's largest during the Holocene and produced the thin but widespread phreatoplinian Taupo Ignimbrite, which covered 20,000 km2 of North Island.
Eruption history
25 recordedGlossaryDetailed timeline
- 260VEI 0Geological estimate260 – end unknownEast Lake Taupo (Horomatangi Reefs)
- 233 (±13 yrs)VEI 6Geological estimate233-03-15 – end unknownHoromatangi Reefs area
- 200 BCEVEI 4Geological estimate200 BCE – end unknown4 km NW of Te Kohaiakahu Point
- 800 BCEVEI 2Geological estimate800 BCE – end unknownOuaha Hills
- 1010 BCE (±200 yrs)VEI 4Geological estimate1010 BCE – end unknown4 km NW of Te Kohaiakahu Point
- 1050 BCEVEI 4Geological estimate1050 BCE – end unknown5 km NE of Motutaiko Island
- 1250 BCEVEI 3Geological estimate1250 BCE – end unknown4 km W of Te Kohaiakahu Point
- 1460 BCE (±40 yrs)VEI 6Geological estimate1460 BCE – end unknownHoromatangi Reefs?
- 2500 BCEVEI 3Geological estimate2500 BCE – end unknown3 km SW of Motutaiko Island
- 2600 BCEVEI 4Geological estimate2600 BCE – end unknown3 km NW of Te Kohaiakahu Point
- 2800 BCEVEI 3Geological estimate2800 BCE – end unknown
- 2850 BCEVEI 3Geological estimate2850 BCE – end unknown2 km S of Te Tuhi Point
- 2900 BCEVEI 4Geological estimate2900 BCE – end unknown5 km NW of Te Kohaiakahu Point
- 3070 BCEVEI 4Geological estimate3070 BCE – end unknown5 km NW of Te Kohaiakahu Point
- 3120 BCEVEI 3Geological estimate3120 BCE – end unknown2 km W of Te Kohaiakahu Point
- 3170 BCE (±200 yrs)VEI 4Geological estimate3170 BCE – end unknown4 km NW of Te Kohaiakahu Point
- 3420 BCEVEI 3Geological estimate3420 BCE – end unknown
- 4000 BCEVEI 3Geological estimate4000 BCE – end unknown
- 4100 BCEVEI 4Geological estimate4100 BCE – end unknown4 km WNW of Kohaiakahu Point
- 4700 BCEVEI 4Geological estimate4700 BCE – end unknownEast-central Lake Taupo
- 5100 BCEVEI 3Geological estimate5100 BCE – end unknownSE Lake Taupo (Motutaiko Island) (Unit F)
- 8130 BCE (±200 yrs)VEI 5Geological estimate8130 BCE – end unknownCentral, E-central L. Taupo (Opepe)
- 9210 BCEVEI 4Geological estimate9210 BCE – end unknownAcacia Bay lava dome
- 9240 BCE (±75 yrs)VEI 5Geological estimate9240 BCE – end unknown4 km W of Te Kohaiakahu Point
- 9460 BCE (±200 yrs)VEI 5Geological estimate9460 BCE – end unknownEast-central Lake Taupo (Karapiti)
Nearby volcanoes
External links
⚠ For reference only. Not for emergency response.