Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
A persistent weak layer of faceted snow that developed during the cold dry period in mid November exists on aspects that face W-N-SE. The greatest danger exists on slopes facing NW-N-E, where wind drifted snow has built thick slabs on top. These hard slabs are 1-4' thick and can produce very large, deep, and potentially deadly avalanches. Out of the wind zone an active weather pattern throughout December has stacked plenty of storm snow and built a cohesive and well connected slab on top of the weak, sugary, faceted snow. This weak layer has become less reactive in recent stability tests (for more details see my obs from Monday). Obvious signs of instability are becoming harder to find each day. What hasn't changed is the poor snowpack structure. Likely places to trigger an avalanche right now include:
- Slope margins where the slab is more thin and the weight of a rider is more likely to trigger the weak layer
- Shallow, rocky areas with a thin snowpack
- Steep convex rollovers
You can avoid this avalanche problem by keeping your slope angles below 30 degrees, ride slopes that are heavily anchored by dense trees, or ride South facing slopes that do not harbor this dangerous persistent weak layer.
This video was shot Monday 12-19.