Journal of Geography (Chigaku Zasshi)
Online ISSN : 1884-0884
Print ISSN : 0022-135X
ISSN-L : 0022-135X
The 100s: Significant Exposures of the World (No.12)
The Taupō Eruption Sequence of AD 232 ± 10 in Aotearoa New Zealand: A Retrospection
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2021 Volume 130 Issue 1 Pages 117-141


 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 to Y5) followed by the extremely violent emplacement of a low-aspect-ratio ignimbrite (unit Y6). The fall deposits include three phreatomagmatic units, Y1, Y3, and Y4, the latter two being the products of archetypal phreatoplinian events; and two magmatic units, Y2 and Y5, the latter being the product of an exceptionally powerful plinian (previously described as ‘ultraplinian’) event with an extreme magma discharge rate around 108 to 1010 kg s−1. The pyroclastic fall-generating eruptions were followed by the climactic emplacement of the entirely non-welded Taupō ignimbrite (Y6). It was generated by the catastrophic collapse of the 35 to 40-km-high plinian eruption column (Y5) that produced a very-fast-moving (600 to 900 km h−1), hot (up to 500°C) pyroclastic flow (density current) that covered about 20,000 km2 of central North Island over a near-circular area ∼160 km in diameter, centred on Lake Taupō, in fewer than about ten to 15 minutes. This violent ground-hugging pyroclastic flow generated its own air lubrication, forming a near-frictionless basal region, and the resultant highly fluidised ignimbrite was spread as a near-continuous but thin sheet over the entire landscape, both infilling valleys and mantling ridges. Caldera collapse formed a new basin in the older Ōruanui caldera in Lake Taupo. The pressure-wave arising from the plinian-column collapse probably generated a global volcano-meteorological tsunami. Studied intensely by extraordinary volcanologists Colin Wilson and George Walker, and others, the exceptionally well-preserved and readily-accessible Taupō eruptives provide a one-in-a-hundred classic sequence that is arguably the most informative in the global world of volcanology with respect to explosive rhyolitic eruptions and their products. The total volume of the Taupō eruptives amounts to ∼35 km3 as magma, equivalent to ∼105 km3 of bulk (loose) pyroclastic material, of which the Taupō ignimbrite comprises ∼30 km3. The impacts and landscape response of the eruption were profound, spatially extensive, and enduring, and the young glassy soils (Vitrands in Soil Taxonomy, Pumice Soils in the New Zealand Soil Classification) developed in the silica-rich pumiceous deposits, although well suited to plantation forestry (especially exotic Pinus radiata), pose unique problems for agriculture and other land uses, including a high susceptibility to gully erosion and an inherent deficiency in cobalt and other trace elements, and require special management.

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