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The AD 186 eruption at Taupo is considered to be the most violent and explosive known. About 9 cubic km of pumice was erupted and eruption column heights reached 45-50 km (about twice the height of Vesuvius 79 AD). Ash was distributed over an extremely large area. 50 km downwind the deposit is 1 m thick. At 100 km it is more than 25 cm thick and pumice clasts are up to 3 cm in diameter (compared to 1 cm for Vesuvius 79 AD). Walker (1980) described the eruption as ultraplinian.