Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
January and February were dry months. During this time weak layers formed throughout the forecast area. In the month of March a series of storms slowly built up slabs that have the potential to activate those weak layers. These weak layers are between 1-2 feet deep. While there has been only minimal activity on these layers, the potential exists. This avalanche problem is more likely to be encountered in steep upper elevation terrain on the north half of the compass and in terrain that avalanched in early January.