The Taupō eruption sequence of AD 232 +- 10 in Aotearoa New Zealand: a retrospection

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Title

The Taupō eruption sequence of AD 232 +- 10 in Aotearoa New Zealand: a retrospection

Content partner

University of Waikato

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ResearchCommons@Waikato

Description

The Taupō eruption, also known as eruption Y, occurred in late summer to early autumn (typically late March to early April) in AD 232 +- 10 yr at Taupō volcano, an ‘inverse’ caldera volcano underlying Lake Taupō in the central Taupō Volcanic Zone, North Island, Aotearoa New Zealand. The complex rhyolitic eruption, the most powerful eruption globally in the last 5000 years, lasted between several days and several weeks and generated five markedly contrasting pyroclastic fall deposits (units Y1...

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Format

Research Paper

Research format

Journal article

Date created

2021-02-25

Creator

Lowe, David J. / Pittari, Adrian

URL

https://hdl.handle.net/10289/16150

Related subjects

Taupō eruption, Taupō supervolcano, eruption Y, non-welded ignimbrite, low-aspect ratio ignimbrite, inverse volcano, pyroclastic flow, density current, plinian, phreatoplinian, radiocarbon wiggle-matching, breakout flood, rhyolite, tephrochronology, tephra, Vitrands, Pumice Soils, volcanic hazard, Taupō Volcanic Zone, gullying, cobalt deficiency, plantation forestry

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