Avalanche

What is an avalanche? An avalanche is a rapid movement of snow down a steep mountainside. Avalanches are extremely powerful, contain millions of tonnes of material, and can move at over 300 km/hr. They mainly occur in spring when snow thicknesses are greatest and when the ice begins to melt and become slippery.

An avalanche speeding down a mountainside.
Avalanches can only be prevented by building fences across the mountainside, as shown in this picture.

Avalanches are most common on slopes between about twenty and forty degrees. Any gentler than this, and snow tends not to move. Any steeper, and the snow does not build up in the first place.

Avalanches are most common in spring, when there is sometimes a warm day that melts the surface of the ice (which later refreezes during the night) and cold days when snow falls.

The layers of ice and new snow are very unstable, like a pack of cards on a steep slope. The point is, you never know when the avalanche will begin, and it can be triggered by something as simple as a loud shout.

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