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A rock avalanche is a geological phenomenon where a large mass of rock fragments rapidly descends a steep slope. These events are a type of debris avalanche, characterized by their high water content, which allows them to behave similarly to snow avalanches.123

Avalanches, in general, occur when material on a slope breaks loose and quickly gathers more material as it moves downhill. While snow avalanches are common, rock avalanches, ice avalanches, and debris avalanches (containing a mix of materials like stones and soil) also exist. The occurrence of any avalanche depends on factors such as terrain, weather, and the stability of the material on the slope.1

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