Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
A buried persistent weak layer that formed in November is present on all aspects in the La Sal range. The big New Year's storm produced several large and destructive avalanches near treeline and above on slopes that face NW-N-NE. Blowing and drifting snow is continuing to add stress to these slopes and you will find the greatest danger on the North half of the compass. Recent stability tests have shown that the weak layer is gaining strength. Avalanches are becoming harder to trigger on this layer, but the consequences remain the same. Any avalanche triggered on the deeply buried PWL would be massive and devastating.
Signs of instability have become less obvious as we get further away from our last loading event. The very large crowns and debris piles around Gold Basin should be a good reminder of what is lurking under the snow. Most accidents occur when the danger is moving from Considerable to Moderate, keep this in mind today.