Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Unlikely
- Taille
- 2
Weak, sugary, faceted snow still exists near the ground, mostly above treeline on NW-N-E aspects. The most dangerous areas are less than 5' deep and contain wind-drifted snow on top of the deeply-buried persistent weak layer. Slopes with steep convexities and rocky, more radical terrain are where you are most likely to trigger an avalanche failing on weak, faceted snow. Here is a classic example of where this avalanche problem currently exists:
A lot of terrain in this photo remains problematic. Rock bands, steep convexities, and thin snowpack areas abound. These are likely trigger points for an avalanche where even a relatively small slide could have devastating consequences. The complex terrain features are also subject to wind-loading and cross-loading can occur from a variety of wind directions.