Mayor Island volcano

Shield volcano 355 m / 1,165 ft
New Zealand, -37.28°S / 176.25°E
Current status: normal or dormant (1 out of 5)

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Typical eruption style: unspecified
Mayor Island volcano eruptions: 5060 BC ± 200 years

Latest nearby earthquakes

TimeMag. / DepthDistance/Location
Mon, 21 Jun 2021 (GMT) (1 earthquake)
21 Jun 2021 05:22:54 GMT
2.7

217 km
36 km (22 mi)
South Pacific Ocean, 38 km northeast of Tauranga, Bay of Plenty, New Zealand
Fri, 18 Jun 2021 (GMT) (2 earthquakes)
18 Jun 2021 09:31:08 GMT
2.1

112 km
23 km (14 mi)
South Pacific Ocean, 30 km north of Tauranga, Bay of Plenty, New Zealand
18 Jun 2021 00:51:51 GMT
2.6

163 km
39 km (24 mi)
South Pacific Ocean, 62 km northeast of Tauranga, Bay of Plenty, New Zealand
Sat, 12 Jun 2021 (GMT) (1 earthquake)
12 Jun 2021 16:30:18 GMT
1.9

222 km
50 km (31 mi)
South Pacific Ocean, 86 km northeast of Tauranga, Bay of Plenty, New Zealand
Wed, 9 Jun 2021 (GMT) (1 earthquake)
9 Jun 2021 17:52:45 GMT
1.8

196 km
32 km (20 mi)
South Pacific Ocean, 36 km northeast of Tauranga, Bay of Plenty, New Zealand

Background

The small 4-km-wide Mayor Island, also known as Tuhua, in the Bay of Plenty is the emergent portion of a 15-km-wide compound peralkaline lava shield constructed between about 120,000 and 35,000 years ago. A 3-km-wide composite caldera was formed in two or three collapse events, the last of which took place about 6300 years ago, and was accompanied by a plinian eruption that produced tephra deposits up to 70 cm thick on mainland North Island. Post-caldera eruptions generated a series of lava domes and flows emplaced from NNE-trending vents within the caldera that have filled it to depths of at least 180 m. The latest eruption of Mayor Island has not been dated, but was considered by Houghton et al. (1992) to perhaps have occurred only 500-1000 years ago.
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Smithsonian / GVP volcano information


See also: Sentinel hub | Landsat 8
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