Abstract
The Tarawera Volcanic Complex comprises 11 rhyolite domes and associated flows and one plug. These extrusions, together with pyroclastic debris, were formed during the Rerewhakaaitu eruption (14,700 ± 400 yr before 1960), the Waiohau eruption (11,250 ± 250 yr before 1960), and the Kaharoa eruption (930 ± 70 yr before 1960). The Tarawera eruption of 10 June 1886 was basaltic, forming the Tarawera Basalt, and terminating in a violently explosive phase which left a linear series of craters cutting three of the rhyolite domes, and providing good internal sections.

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