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Mangakino Volcano

Updated: Apr 20, 2024 05:21 GMT -
Caldera 1165 m / 3822 ft
New Zealand, -38.35°S / 175.75°E
Current status: (probably) extinct (0 out of 5)

[smaller] [larger]
Typical eruption style: unspecified
Mangakino volcano eruptions: None during the past 10,000 years
Less than 2.58 million years ago (Pleistocene)

Latest nearby earthquakes

TimeMag. / DepthDistance / Location
Apr 12, 08:20 am (Auckland)
2.7

148 km
17 km (10.3 mi) to the NE New Zealand
Info
Wednesday, April 10, 2024 GMT (1 quake)
Apr 11, 04:00 am (Auckland)
3.1

161 km
30 km (18 mi) to the S New Zealand
Info
Thursday, April 18, 2024 GMT (1 quake)
Apr 19, 03:30 am (Auckland)
2.6

223 km
19 km (12 mi) to the NE New Zealand
Info
Saturday, April 6, 2024 GMT (1 quake)
Apr 7, 10:12 am (Auckland)
2.6

136 km
24 km (15 mi) to the NE New Zealand
Info
Friday, April 19, 2024 GMT (2 quakes)
Apr 20, 12:01 am (Auckland)
2.5

138 km
25 km (15 mi) to the SE New Zealand
Info
Apr 20, 10:05 am (Auckland)
2.4

184 km
12 km (7.6 mi) to the NW New Zealand
Info

Background

The Pleistocene Mangakino volcanic center has been the source of large-volume rhyolite ignimbrites erupted between 1.6 and 0.9 million years ago (Ma) (Wilson et al., 1984; Houghton et al., 1995). Two principal periods of activity occurred, from 1.6 to 1.53 Ma and 1.21 to 0.9 Ma (Wilson et al., 1995a). One of the largest ignimbrite eruptions of the Taupo volcanic zone took place at 1.21 Ma from Mangakino. The Titiraupenga and Pureora andesitic lava domes lie just to the south of the inferred caldera margin.
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Source: Smithsonian / GVP volcano information

Latest satellite images

mangakino satellite image sat1mangakino satellite image sat2
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