Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
Weak layers in the upper snowpack caused natural avalanche activity during the last storm and a string of human-triggered avalanches each day since. A layer of facets and facet-crust combination exist 1 to 3 feet deep and represent the most likely place for a Persistent Slab to release. Avalanches could release naturally from wind loading or be remotely triggered below or adjacent to steep slopes. As snow accumulates, the potential avalanche size will increase from recent days. The best way to manage this problem is through lower-angled terrain and managing your exposure to overhead hazards.
A remotely triggered avalanche from Sunday on the northeast slopes of Schuylkill Ridge. Expect slopes like this to become dangerous today, with the avalanche size increasing as snow accumulates through out the day.