Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 1–2
The rapidly accumulating snow, combined with strong winds, will form storm slabs that can be easily triggered by a skier anywhere in the mountains. These slabs will rest on a crust that is likely to provide an excellent sliding surface, which could increase their reactivity. The danger will be particularly pronounced on north-facing leeward slopes. Strong winds could create reactive slabs lower down the mountain than usual.