Item talk:Q238016
From geokb
{
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Deposits of one such event in the southwestern USA, the 18.8 Ma Peach Spring Tuff, were formed by pyroclastic flows that travelled >170\u2009km from the eruptive centre and entrained blocks up to ~70\u201390\u2009cm diameter from the substrates along the flow paths. Here we combine these data with new experimental results to show that the flow\u2019s base had high-particle concentration and relatively modest speeds of ~5\u201320\u2009m\u2009s\u22121, fed by an eruption discharging magma at rates up to ~107\u2013108\u2009m3\u2009s\u22121\u00a0for a minimum of 2.5\u201310\u2009h. 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