Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Many areas of the Togwotee Pass forecast zone have poor snowpack structure. In many of those areas snow that fell in January and February lies upon a weak base of well-developed faceted snow crystals. Other persistent weak layers include buried layers of surface hoar and near surface faceted snow. Large slab avalanches with depths from 1 to 3 feet could be triggered by the weight of a single person on these weaknesses.