Pyroclastic flows are fast-moving currents of hot gas and volcanic matter (such as ash, pumice, and rock fragments) that flow down the slopes of a volcano during an eruption. They are extremely dangerous and can travel at speeds of up to 700 km/h, reaching temperatures of 1,000°C or more.
Pyroclastic flows are typically triggered by a collapse of rapidly rising volcanic plumes, or by the explosive release of gas and volcanic material during a volcanic eruption. The collapse of a volcanic dome or the eruption column can generate a pyroclastic flow as well.
By studying pyroclastic flows, we can gain a deeper understanding of the complex and powerful forces at work within our planet, and develop strategies to protect vulnerable communities from the impacts of volcanic activity.