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    Glossary

    Pyroclastic Flow

    A pyroclastic flow is a mixture of scorching gas, ash and rock that races down the slopes of a volcano. It can exceed 100 km/h and several hundred degrees.

    It is the deadliest volcanic hazard. It cannot be outrun once it starts, hence the importance of evacuating in advance. It destroyed Pompeii in AD 79 and Saint-Pierre in Martinique in 1902.

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