Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2–3.5
Two weak layers exist within the upper snowpack: the mid-February layer (down 70 to 120 cm) and the mid-January layer (down 100 cm). They both consist of surface hoar / melt-freeze crust. Evidence of their reactivity has been observed consistently all week. With increased load from the current storm and warmer temperatures, they have the potential to "wake up" and produce large, unexpected avalanches. In times of uncertainty, choose simple terrain, low consequence slopes and conservative lines.