Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
Isolated collapsing yesterday indicates that the recent snow load has begun to stress persistent weak layers buried deep in the snowpack. The snowpack structure is poor with a dense hard slab 2-3 feet thick on top of multiple layers of weak, sugary, faceted snow. Stability tests remain reactive but stubborn. Nevertheless, any avalanche triggered would be deep, dangerous, and possibly un-survivable. The danger is greatest on steep slopes near and above treeline where strong, southwest winds have deposited thick slabs on top of these weak layers and this type of terrain should be avoided. Northerly aspects below treeline also remain suspect with equally poor structure. The main difference is a lack of recent wind loading. In these areas, deep, human triggered avalanches remain possible.