INTRODUCTION
TYPES
OF AVALANCHE
THE
MECHANISM OF AVALANCHE RELEASE
FORECASTING
SNOW AVALANCHES
AVALANCHE
CONTROL TECHNIQUES
AVALANCHE
HAZARD RATINGS
AVALANCHE
TRAINING FOR DOGS
INFO
ON THE PAGE OWNERS
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TYPES
OF AVALANCHE...
Loose snow avalanches are formed
in snow which have little internal cohesion among individual snow crystals.
When such snow lies in a state of unstable equilibrium on a slope steeper
than its natural angle of repose, a slight disturbance is enough to set
snow in downhill motion progressively. If enough momentum is generated,
the sliding snow may run out onto level ground, or even ascend an opposite
valley wall. Such an avalanche originates at a point, growing wider as
it sweeps up more snow in its descent. The demarcation between sliding
and undisturbed snow is diffuse, especially in dry snow.
Three processes commonly leave snow
in a state of unstable equilibrium on a slope
steeper than its natural angle of repose: (1)
Deposition of stellar or dendritic crystals with
little or no wind, (2) reduction of internal
cohesion among crystals by metamorphism, and
(3) reduction of internal cohesion by intrusion
of liquid water. Though very numerous, most dry
loose snow avalanches are small and few achieve
sufficient size to cause damage. With advent
of spring melting, wet loose snow avalanches
also are common. Most of the latter, too, are
small, but they are more likely to develop occasional
destructive size, especially when confined to
gulleys.
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Picture Gallery
In this section, you will
get to see pictures of avalanches happening worldwide...dated from the
1900...
Maps of avalanche-affected
areas
Click on the globe to see
frequently hit places...
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