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Avalanches are caused by the accumulation and bonding of snow layers, becoming unstable due to weak bonds and sudden environmental changes. The ideal slope for avalanches is between 30-40 degrees, and preventive measures include monitoring, controlled detonations, and avoiding hazardous areas. There are two main types of avalanches: loose snow avalanches, which start from a single point, and slab avalanches, which are more dangerous and involve larger cohesive snow layers.

Author

18walesi

Language

EN