Pompeii eruption, Mount Vesuvius, pyroclastic flows, and volcanic physics explained.
In 79 AD, Pompeii was engulfed by a 700°C pyroclastic flow from Mount Vesuvius — a fast-moving avalanche of superheated gas, ash, and volcanic rock.
These pyroclastic density currents behave like a strange hybrid of solid and fluid, where particles become preserved in hot gas and move with terrifying speed. Driven by fluid dynamics, thermal energy, and particle fluidization, these flows can surge across the landscape faster than a hurricane — sometimes approaching supersonic speeds.
The result?
A violent geological event that instantly encapsulated Pompeii, preserving people, buildings, and everyday objects in a chilling snapshot of Roman life nearly 2,000 years ago.
In this video we break down the physics behind pyroclastic flows and how volcanic chaos can create a perfect archaeological time capsule.
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