Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
The widespread persistent weak layer (PWL) that formed in November is showing signs of strengthening and stability tests continue to be less reactive. This means avalanches are becoming harder to trigger but the consequences remain the same. Any avalanche triggered on this deeply buried PWL would be large and unsurvivable. The greatest risk exists on steep, wind drifted slopes with a northerly aspect, but a relatively poor snowpack structure remains on all aspects. Carefull slope assesment and stability analysis is required before venturing into steep terrain. As we start to think about easing into larger terrain, areas to avoid include slopes with steep convexities or blind break-overs; thin snowpack areas along slope margins or near shallowly buried rock outcrops; and areas of steep, rocky, more radical terrain.