Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
Persistent weak layers of loose, sugary, faceted snow are present on many aspects and elevations. On slopes facing NW-N-E-SE, slabs 1'-3' deep exist on top of these weak layers. New and wind drifted snow will further stress these weak layers and deep and dangerous, human-triggered avalanches will become increasingly more likely. The danger increases with elevation, particularly on slopes with recent deposits of wind drifted snow.
The photos below illustrate classically poor snowpack structure with a clearly defined fist to 4 finger hard slab on top of weak, sugary, facets. In other words - strong snow over weak snow. Stability tests indicate a stubbornness to release but this only makes them harder to predict. It's like provoking someone with a violent temper - you don't know when they are going to explode. As long as this snow structure remains in place, I won't be provoking any steep northerly facing slope.