Construct · 1 fields · 1 citations
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A plinian eruption is a highly explosive style in which a sustained, buoyant eruption column rises tens of kilometres into the atmosphere and blankets wide areas with fall deposits, named for Pliny the Younger's account of the 79 CE eruption of Vesuvius. Walker's 1973 classification placed plinian eruptions at the high-dispersal, high-fragmentation end of a scheme that sorts explosive eruptions by how widely and how finely their fall deposits are spread. The referent is an eruption magnitude-and-style category defined by column behaviour and deposit dispersal, distinct from effusive or mildly explosive activity.[1]
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