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Pyroclastic rock refers to fragmented volcanic material ejected during an eruption, classified by size from dust to bombs. These materials are formed when expanding gases shred magma into pieces. Pyroclastic flows are fast-moving, ground-hugging clouds of hot rock fragments, gases, and air, capable of reaching speeds over 100 km/hour and causing immense destruction. They are distinct from lava flows, which are molten rock that moves slowly and solidifies into rock. Ignimbrites and nuées ardentes are types of deposits left by pyroclastic flows.1

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  1. pyroclastic flow
  2. igneous rock

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