May 24, 2013
Winter 2012 - 2013



Kinds of Avalanches

Avalanches come in many shapes and sizes. In general, there are two types for snowmobilers to consider:

1) Dry slab avalanches: Most fatalities occur in dry slab avalanches. These types quickly fracture over wide areas with the victim often caught in the middle. Dry slab avalanches can even be triggered from FLAT TERRAIN at near the bottom of the slope.

Fractures can propagate through the snow at speeds of 50-200 mph. People can sometimes escape but most do not.

When climbing snowmobilers frequently do not have the ability or momemtum to get off the moving slab. Occasionally riders can escape the slab when descending and near the bottom.

See Anatomy of a Slab Avalanche below...


2) Wet avalanches: These types occur when warm temperatures weaken the bonds between layers in the snowpack. Wet avalanches sometimes look like concrete quickly pouring down a slope. Look for them:

  • If temperatures have been above freezing for extended periods.
  • When daytime temperatures rise rapidly and snowballs or pinwheels begin rolling down slopes.
  • If you squeeze a hand full of snow and it makes your glove wet or if water literally drips out of the snow

 





Anatomy of a Slab Avalanche
Mouse over the terms below and get the definition for each

The top fracture surface of a slab avalanche. Usually smooth, clean cut, and angled 90 degrees to the bed surface. The surface over which a fracture and subsequent avalanche release occurs. Can be either the ground or a snow surface. The portion of an avalanche path where an avalanche releases. The portion of an avalanche path between the starting zone and the runout zone. The portion of an avalanche path where the debris typically comes to rest.



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