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Mangakino Volcano

Updated: 8 мая 2024 14:07 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

ВремяМагнитуда / ГлубинаРасстояние / Местоположение
6 мая 22:04 (Auckland)
2.4

78 km
19 km к северу New Zealand
Более
Воскресенье, 5 мая 2024 GMT (1 земл.)
5 мая 16:02 (Auckland)
3.0

130 km
29 km к юго-востоку New Zealand  I FELT IT
Более
Четверг, 2 мая 2024 GMT (2 земл.)
2 мая 18:57 (Auckland)
2.2

133 km
New Zealand
Более
2 мая 14:46 (Auckland)
2.2

107 km
New Zealand
Более
Вторник, 30 апреля 2024 GMT (1 земл.)
1 мая 10:21 (Auckland)
2.9

172 km
17 km к северо-востоку New Zealand
Более
Среда, 24 апреля 2024 GMT (1 земл.)
25 апр 11:11 (Auckland)
2.9

146 km
5.8 km к югу New Zealand
Более

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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