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The
Pinatubo is, like Mount Mayon, a strato volcano. This type of volcano is
steep-sided and composed of alternating layers (layer = strata)
of lava and other volcanic
material, especially volcanic ash.
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Pyroclastic
flows
(flows with mixtures of hot, dry rock fragments and hot gases.
They result from the
explosive eruption of molten or solid rock fragments, or both)
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Tephra
(fragments of volcanic rock and
lava regardless of size, which are blasted into the air by explosions or
carried upward by hot gases)