Weak Layer:
All snow exists as layers. Some layers are relatively more cohesive
(stronger layers) and others are relatively less cohesive (weaker
layers). Like cliffs in the Grand Canyon, if you brush a snowpit
wall with your mitten, the weaker layers erode away while the
stronger layers stick out. When the snowpack is stressed by
rapid changes (e.g. wind-drifted snow, new snow, or rain)
this stress can cause the weak layer to fracture. Understandably, most avalanche geeks are
obsessed by weak layers. Weak layers involved in most avalanche
accidents usually are a “persistent” grain type
such as faceted snow, surface hoar or depth hoar, but it can
also be a layer formed within new snow such as low density new
snow or graupel. After an avalanche occurs, you often hear avalanche
professionals ask, “what was the weak layer” or
“what did it run on?” The life of an avalanche aficionado
revolves around knowing what is the weakest layer in the snowpack
and how much stress it takes to make it fail. |
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