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There are no activity reports for Mayor Island.
Available Weekly Reports
There are no Weekly Reports available for Mayor Island.
Summary of eruption dates and Volcanic Explosivity Indices (VEI).
|Start Date||Stop Date||Eruption Certainty||VEI||Evidence||Activity Area or Unit|
|5060 BCE ± 200 years||Unknown||Confirmed||5||Radiocarbon (corrected)||South end of caldera, Taratimi Bay|
|6050 BCE ± 75 years||Unknown||Confirmed||Radiocarbon (uncorrected)||SE caldera rim|
The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.
Buck M D, 1985. An assessment of volcanic risk on and from Mayor Island, New Zealand. New Zeal J Geol Geophys, 28: 283-298.
Buck M D, Briggs R M, Nelson C S, 1981. Pyroclastic deposits and volcanic history of Mayor Island. New Zeal J Geol Geophys, 24: 449-468.
Ewart A, Taylor S R, Capp A C, 1968. Geochemistry of the pantellerites of Mayor Island, New Zealand. Contr Mineral Petr, 17: 116-140.
Gottsmann J, Dingwell D B, 2002. The thermal history of a spatterfed lava flow: the 8-ka pantellerite flow of Mayor Island, New Zealand. Bull Volc, 64: 410-422.
Houghton B F, Weaver S D, Wilson C J N, Lanphere M A, 1992. Evolution of a Quaternary peralkaline volcano: Mayor Island, New Zealand. J Volc Geotherm Res, 51: 217-236.
Houghton B F, Wilson C J N, 1986. Explosive rhyolite volcanism: the case studies of Mayor Island and Taupo volcanoes (Tour Guide A1). New Zeal Geol Surv Rec, 12: 33-100.
IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..
Lowe D J, Shane P A R, Allowayc B V, Newnham R M, 2008. Fingerprints and age models for widespread New Zealand tephra marker beds erupted since 30,000 years ago: a framework for NZ-INTIMATE. Quat Sci Rev,.
Shane P, Sikes E L, Guilderson T P, 2006. Tephra beds in deep-sea cores off northern New Zealand: implications for the history of Taupo Volcanic Zone, Mayor Island and White Island volcanoes. J Volc Geotherm Res, 154: 276-290.
Stevenson R J, Briggs R M, Hodder A P W, 1993. Emplacement history of a low-viscosity, fountain-fed pantelleritic lava flow. J Volc Geotherm Res, 57: 39-56.
Wilson C J N, Houghton B F, Pillans B J, Weaver S D, 1995. Taupo Volcanic Zone calc-alkaline tephras on the peralkaline Mayor Island volcano, New Zealand: identification and uses as marker horizons. J Volc Geotherm Res, 69: 303-311.
The small 4-km-wide Mayor Island, also known as Tuhua, in the Bay of Plenty is the emergent portion of a 15-km-wide compound peralkaline lava shield constructed between about 120,000 and 35,000 years ago. A 3-km-wide composite caldera was formed in two or three collapse events, the last of which took place about 6300 years ago, and was accompanied by a plinian eruption that produced tephra deposits up to 70 cm thick on mainland North Island. Post-caldera eruptions generated a series of lava domes and flows emplaced from NNE-trending vents within the caldera that have filled it to depths of at least 180 m. The latest eruption of Mayor Island has not been dated, but was considered by Houghton et al. (1992) to perhaps have occurred only 500-1000 years ago.