Rotoiti caldera

E827899

Rotoiti caldera is a large volcanic depression in New Zealand’s central North Island, formed by major explosive eruptions within the Okataina Volcanic Centre.

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All labels observed (2)

Label Occurrences
Okataina Caldera 1
Rotoiti caldera canonical 1

Statements (36)

Predicate Object
instanceOf caldera
geological formation
composition rhyolitic magma
country New Zealand
eruptionStyle Plinian
caldera-forming eruption
formedBy collapse of magma chamber
explosive eruptions
silicic volcanism
geologicalAge Pleistocene NERFINISHED
Quaternary
hasRockType ignimbrite
rhyolitic tuff
hasSignificance major Quaternary caldera of New Zealand
hazardType explosive volcanism
isPartOf Okataina volcanic complex NERFINISHED
isWithin Okataina Caldera Complex NERFINISHED
lastEruptionPeriod Late Pleistocene
locatedIn Bay of Plenty Region NERFINISHED
New Zealand volcanic plateau NERFINISHED
North Island
Taupō Volcanic Zone NERFINISHED
central North Island
locatedNear Lake Rotoiti NERFINISHED
Rotorua NERFINISHED
locatedOn continental crust
nearbyFeature Okataina caldera NERFINISHED
Rotorua caldera NERFINISHED
partOf Okataina Volcanic Centre NERFINISHED
produced Rotoiti Ignimbrite NERFINISHED
widespread tephra deposits
region central North Island volcanic plateau
scientificDiscipline geology
volcanology
tectonicSetting subduction-related arc volcanism
volcanicArcOrBelt Taupō Volcanic Zone NERFINISHED

Referenced by (2)

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

Okataina Volcanic Centre hasSubfeature Rotoiti caldera
Taupō Volcanic Zone contains Rotoiti caldera
this entity surface form: Okataina Caldera