Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
Faceted snow and melt-freeze crusts formed during an extended dry period that ended on December 11th. Since that time, the higher elevations of the Tetons have received close to four inches of snow water equivalent. Slabs that could be soft or hard can be triggered in avalanche terrain with depths to three feet at the higher elevations and to eighteen inches at the low elevations. Be particularly wary of unsupported slopes and cliff areas.