Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 2–3
We've been plagued by persistent weak layers the entire season. First by early-season facets near the ground, then by weak layers that were buried in late-January and February. Warm temperatures and a lack of loading over the past week have finally given these layers a bit of a breather. These weak layers still exist on most slopes, but observations from across the forecast area indicate that triggering a persistent slab avalanche is unlikely.
Even though triggering a persistent slab avalanche is unlikely, that's different from impossible. These weak layers exist on nearly all slopes and if you commit to entering avalanche terrain you should know that they are under your feet or sled. There's still a small chance of triggering a persistent slab avalanche on steep, rocky, wind-affected slopes. The photo at right/above is a good example of this sort of terrain.
ADDITIONAL DISCUSSION:A solid freeze last night and cloud cover today should keep wet snow issues at bay. With that said, this area has a way of dodging clouds ("there's a reason they call it Sun Valley", as folks like to say). If you find yourself sinking into wet snow it's a good time to think about finding a colder slope to play on.
There's still a small chance of triggering a persistent slab avalanche, primarily in terrain like shown in the photo—very steep, rocky, and wind-affected. Johnstone Peak area.