Avalanche
Avalanche is also called Snowslide and it occurs when there is a rapid flow of snow down a hill or mountain slope after the breaking of an unstable mass of snow. This sudden flow of snow slides down very quickly taking more snow along with it, getting bigger in size, and becomes dangerous. Avalanches can be triggered by a number of factors, such as increased precipitation or weakening of the snowpack, or interference from external means such as humans, animals, and earthquakes. Sometimes these Avalanches drag not only snow and wind with them but also whatever comes on their way. Avalanches normally occur in spring or winter.
Avalanches may occur in four different forms. Slab Avalanche, Loose Snow Avalanche, Powder Snow Avalanche, and Wet Snow Avalanche. The slab avalanches are triggered by the collapse of an underlying weak snow layer and the loose avalanches are made of loose snow that have a milder impact. Wet snow avalanches are often triggered by rain and abundant sunshine, which weakens the strength of the snowpack. Avalanches usually move very fast and if an avalanche moves fast enough, some of the snow may mix with the wind, causing a powder snow avalanche.
Avalanches bring a huge amount of devastation in mountainous areas, due to which life there comes to a standstill. Therefore, a lot of efforts have been put into avalanche control. Avalanches are usually different from mudflows, rock slides, mudslides, and serac collapses. These catastrophic events come suddenly and can be fatal. In 1970, a deadly avalanche of ice and rocks devastated the town of Yungay, Peru, killing 22,000 people.
Landslide
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