Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 3
Our main avalanche problem continues to be the persistent weak layers (PWL) that formed in November and December. We saw widespread natural avalanche activity on these layers at the beginning of the month. Our last storm wrapped up on February 9th. With each passing day, it becomes less likely to trigger an avalanche on the PWL, but any avalanche triggered would be life-threatening. At this point, you will not get any feedback from the snow, collapsing and cracking are long gone. You may start seeing tracks in bigger, more consequential terrain. It is important to remember that tracks are not an indication of stability. Hard slab avalanches failing on persistent weak layers are often triggered by the third, sixth, or even tenth rider on a slope, wiping out all previous tracks. You should evaluate each slope on an individual basis. Aim to ride in areas with a deep snowpack. Avoid steep, rocky terrain, thinner areas along slope margins, and steep, blind roll overs or convexities. These are all likely trigger points.