Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 3
Our current snowpack is rife with persistent weak layers and in many areas, it's faceted through to the ground. The most prominent weak layers of concern are 1) a layer of near surface facets beneath the most recent storm snow, and 2) faceted snow beneath the Christmas Rain Crust (CRC). Weak snow alone does not constitute a problem, however, we need to have a slab on top of the weak layer. You are most likely to find a slab over top of a weak layer in wind affected terrain near and above treeline on slopes facing N-NE-E. Outlying areas may include slopes facing W, NW, and SE. Slabs triggered in the upper portion of the snowpack have the potential to step down beneath the CRC causing a deeper and much more dangerous avalanche. Without obvious signs of instability, these dangerous avalanches are difficult to predict and the only sure way to avoid them is to avoid slopes steeper than 30 degrees. For more on this structure, see the video below.