Oruanui eruption of Taupō volcano

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The Oruanui eruption of Taupō volcano was a massive supereruption about 26,500 years ago that created Lake Taupō and is one of the largest known volcanic eruptions on Earth in the last 100,000 years.

All labels observed (2)

Label Occurrences
Oruanui eruption 2
Oruanui eruption of Taupō volcano canonical 1

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf caldera-forming eruption
plinian eruption
supereruption
ashDispersal ash detected in marine cores in the South Pacific Ocean
ash dispersed over much of New Zealand
ash identified in Antarctic ice cores
associatedWith Taupō Volcanic Zone rifting
subduction of the Pacific Plate beneath the Australian Plate
climateImpact short-term global climatic cooling likely
continent Oceania
country New Zealand
created Lake Taupō
surface form: Lake Taupō basin

Taupō volcano
surface form: Oruanui caldera
depositThickness ignimbrite locally more than 200 metres thick
eruptionAge Late Pleistocene
about 26,500 years ago
eruptionAgeBP approximately 25,400 radiocarbon years BP
eruptionDuration likely weeks to months (order of magnitude)
eruptionMagnitude M8.8 (approximate)
eruptionOf Taupō volcano
eruptionStyle multi-phase eruption
eruptionVEI 8
eruptionVolume about 1,170 cubic kilometres of magma (commonly cited)
more than 1,000 cubic kilometres of magma
followedBy post-Oruanui eruptive activity at Taupō volcano
hazardRelevance example of potential impacts of supereruptions
hazardType explosive volcanism
locatedIn New Zealand
North Island
Taupō Volcanic Zone
namedAfter Taupō Volcanic Zone
surface form: Oruanui area near Lake Taupō
partOf Taupō volcano
surface form: Taupō Volcanic Centre
precededBy earlier caldera-forming eruptions of Taupō volcano
produced Oruanui ignimbrite
co-ignimbrite ash clouds
pyroclastic density currents
widespread fall tephra deposits
rankedAs largest known eruption of Taupō volcano
one of the largest known eruptions on Earth in the last 100,000 years
researchField tephrochronology
volcanology
resultedIn formation of ignimbrite sheets around Lake Taupō
major enlargement and modification of Taupō caldera
studiedBy GNS Science
surface form: GNS Science (New Zealand)

Quaternary geologists and volcanologists worldwide
tephraVolume more than 1,100 cubic kilometres of tephra
timeScale occurred during Marine Isotope Stage 3–2 transition (approximate)
occurred during the last glacial period
usedFor chronostratigraphic marker in New Zealand Quaternary studies

How these facts were elicited

Referenced by (3)

Full triples — surface form annotated when it differs from this entity's canonical label.

New Zealand volcanic zones notableEruption Oruanui eruption of Taupō volcano
Lake Taupō volcanicEruptionKnownAs Oruanui eruption of Taupō volcano
this entity surface form: Oruanui eruption
Taupō Volcanic Zone notableEruption Oruanui eruption of Taupō volcano
this entity surface form: Oruanui eruption