Rotoiti eruption

E827900

The Rotoiti eruption was a massive late Pleistocene explosive event in New Zealand that produced extensive ignimbrite and caldera-forming activity within the Okataina Volcanic Centre.

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Predicate Object
instanceOf volcanic eruption
affects regional tephrochronology of New Zealand
approximateAge about 45,000 years ago
associatedWith Okataina Caldera NERFINISHED
Okataina Volcanic Centre caldera system NERFINISHED
depositType caldera-fill deposits
ignimbrite
plinian fall tephra
eruptionStyle explosive
followedBy younger Okataina eruptions
formsPartOf central North Island large ignimbrite flare-ups
geologicalPeriod Late Pleistocene
hasNameOrigin Lake Rotoiti area
hasVolcanicExplosivityIndex VEI 7
locatedIn Bay of Plenty Region NERFINISHED
New Zealand NERFINISHED
North Island
Okataina Volcanic Centre NERFINISHED
magnitudeDescription super-eruption scale
partOf Okataina eruptive history
Taupō Volcanic Zone NERFINISHED
precededBy earlier Okataina eruptions
produced Rotoiti ignimbrite NERFINISHED
caldera collapse
extensive pumice fall deposits
widespread ignimbrite sheets
relatedTo Earth’s late Quaternary climate and environmental change studies
studiedIn New Zealand Quaternary volcanology

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Okataina Volcanic Centre notableEruption Rotoiti eruption