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News
Area near yesterday's steam eruption in Rotorua Lake (image: newshub.co.nz / twitter)
Monday, Nov 28, 2016
A small steam explosion (hydrothermal eruption) occurred yesterday in Lake Rotorua. A fountain of water was seen ejected to about 30 m. [read more]. ... [more]
 

Rotorua volcano

Caldera 757 m / 2,484 ft
New Zealand, -38.08°S / 176.27°E
Current status: dormant (1 out of 5) | Reports
Rotorua volcano books
Last update: 28 Nov 2016
Typical eruption style: unspecified
Rotorua volcano eruptions: Pleistocene
TimeMag. / DepthDistanceLocation
Sun, 20 May
Sun, 20 May 20:34 UTCM 3.1 / 69.9 km25 kmNew Zealand
Sun, 20 May 08:28 UTCM 2.3 / 118.4 km10 kmNew Zealand
Sun, 20 May 01:36 UTCM 2.1 / 121.3 km13 kmNew Zealand
Sun, 20 May 00:26 UTCM 2.5 / 120.3 km22 kmNew Zealand
Sun, 20 May 00:26 UTCM 1.8 / 114.7 km26 kmNew Zealand
View all recent quakes

Background:

The 22-km-wide Rotorua caldera is the NW-most caldera of the Taupo volcanic zone. Rotorua is the only single-event caldera in the Taupo volcanic zone and was formed about 220,000 years ago following eruption of the >340 cu km rhyolitic Mamaku Ignimbrite. Although caldera collapse occurred in a single event, the process was complex and involved multiple collapse blocks. The major city of Rotorua lies at the south end of the lake that fills much of the caldera. Post-collapse eruptive activity, which ceased during the Pleistocene, has been restricted to lava dome extrusion without major explosive activity. The youngest eruptive activity at Rotorua consisted of the eruption of three lava domes less than 25,000 years ago. The major thermal areas of Takeke, Tikitere, Lake Rotokawa, and Rotorua-Whakarewarewa are located within the caldera or outside its rim, and the city of Rotorua lies within and adjacent to active geothermal fields.
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Smithsonian / GVP volcano information

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