Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
Persistent weak layers in the middle and at the bottom of the snowpack have temporarily become more reactive on recently wind-loaded slopes at near and above treeline elevations. These slabs are generally hard, will be stubborn to human triggering, but may produce a larger than expected avalanche if released. This avalanche problem has become less common in wind-sheltered areas, with the last notable avalanche having occurred on 2/1.
A large persistent slab that was human triggered on Thursday 2/9 in upper Hunter Creek.