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    Raoul Island

    Stratovolcano · 516 m · New Zealand

    Raoul Island
    Photo: Wikimedia Commons · Public domain · Wikimedia Commons

    Raoul Island sits on the Kermadec Plate, in a subduction zone. 18 eruptions are known since the end of the last ice age, the most recent in 2006. Its major eruptions caused at least 1 deaths.

    Raoul Island is the largest of the Kermadec Islands, north-east of New Zealand. Only a small conservation station is staffed there.

    In March 2006 a sudden explosion in the crater killed a worker who was sampling water there. The island is a reserve for seabirds.

    Elevation
    516 m
    Type
    Stratovolcano
    Tectonic Setting
    Subduction zone, oceanic crust
    Dominant Rock
    Andesite / Basaltic Andesite
    Plate
    Kermadec Plate
    Country
    New Zealand
    Last Eruption
    2006
    Known Eruptions (Holocene)
    18
    Max. Explosivity (VEI)
    6
    Known Fatalities
    1

    Notable Eruptions

    Eruptions that caused deaths or damage, or with an explosivity index of 4 and above (NOAA).

    Eruption Timeline

    Each bar is an eruption; its height shows its explosivity (VEI 0 to 8).

    2000 BCE · VEI 41200 BCE · VEI 4250 BCE · VEI 650 BCE · VEI 3100 · VEI 4400 · VEI 4550 · VEI 4700 · VEI 3850 · VEI 414501630 · VEI 41720 · VEI 41814 · VEI 31870 · VEI 31886 · VEI 01964 · VEI 21987 · VEI 02006 · VEI 1 · deadly eruption VEI 2VEI 4VEI 6 2000 BCE1500180019002000

    Eruption Deadly Eruption (NOAA) Uncertain Date

    Sources : Global Volcanism Program, 2026. Volcanoes of the World (v. 5.4.0; 7 Aug 2026), Smithsonian Institution, doi:10.5479/si.GVP.VOTW5-2026.5.4 (volcano.si.edu) · NOAA NCEI · USGS · Wikidata