The Ohakuri Caldera was formed in a paired single event eruption of Ohakuri ignimbrite and is located in the Taupo Volcanic Zone on the North Island of New Zealand. Its significance was first recognised in 2004, as the geology of the area had been misunderstood until then. The paired eruption resulted in a very large eruption sequence in the Taupō Volcanic Zone about 240,000 years ago that included the formation of Lake Rotorua.
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