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How are volcanic avalanches formed?

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Volcanic avalanches, also known as volcanic landslides or debris flows, are formed when explosive volcanic eruptions release a large amount of volcanic material, such as ash, rocks, and debris. This volcanic material can accumulate on the steep slopes of a volcano's cone or crater. Factors such as gravity, the steepness of the slope, and the amount of material deposited can trigger a rapid collapse, leading to a cascading flow of debris down the volcano's slopes. The force of the moving debris can cause destruction and devastation in the surrounding areas.
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Volcanic avalanches, also known as pyroclastic flows, are formed during explosive volcanic eruptions when hot ash, rock fragments, and gases rapidly flow down the volcano's slopes at high speeds. These flows can reach temperatures of over 1,000 degrees Celsius and are extremely destructive, capable of leveling everything in their path. The force and velocity of the volcanic avalanche are due to the release of pressure from the eruption, causing the material to surge downhill like a fluid, often traveling several kilometers from the volcano.

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