Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2
Persistent slabs lie upon weak, faceted snow and sun crusts formed during the January dry period. There is a high degree of spatial variability associated with these weak layers, which makes them difficult to predict. In some areas the new snow is bonding well to the January surfaces, but that is not the case everywhere. These slabs may be soft or hard and could be triggered by backcountry travelers in steep, avalanche prone terrain with depths of a foot at the lower elevations to four feet at the higher elevations.