Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- 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 between 1-3 feet deep. While there has not been widespread activity on these layers in the Tetons, there have been several avalanches reported in the last week that were large, one of which resulted in a fatality. This avalanche problem is more likely to be encountered in steep mid and upper elevation terrain on the northern half of the compass and in terrain that avalanched in early January. Uncertainty exists around triggering this avalanche type which has not been widespread in the Tetons. Warming may make this avalanche type more easily triggered.