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Pyroclastic flow

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Revision as of 17:36, 10 December 2008 by Muro Bot (talk | changes) (robot Adding: it:Colata piroclastica)

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Pyroclastic flows going down Mayon Volcano, Philippines, in 1984.

A pyroclastic flow is a common result of volcanic eruptions. The flows are currents of hot gas, or tefra, during an eruption that sometimes causes rock falls.

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Volcanology

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