Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Weak layers formed throughout the forecast area during the dry months of January and February. In March, a series of storms built up slabs that in some cases have been large enough to activate those weak layers, making them easier to trigger. These weak layers are one to three feet deep. There have been multiple large natural avalanches and several close calls with machine triggered avalanches involving this layer. This avalanche problem is more likely to be encountered in steep terrain above 8,000' on the northern half of the compass and in terrain that avalanched in early January. Uncertainty exists around triggering this avalanche type but warming will make it easier to trigger.