Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
It's been just over a week since the last storm and avalanche cycle. Red flag signs of instability such as collapsing and cracking are no longer evident, but poor snowpack structure remains. In spite of the warm temperatures and misleading snow surface, layers of weak faceted snow still exist underneath. On northerly aspects near and above treeline, thick hard slabs 2-4 feet thick exist over these persistent weak layers. Although becoming more stubborn to release, when they do they are capable of taking out the entire season's snowpack. Likely trigger points include thin, rocky areas, steep convexities, and areas along slope margins but my strategy continues to be avoidance of steep slopes in these areas entirely.