Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible - Likely
- Size
- 1.5–3
20-60 cm of recent storm snow, warm temperatures, and moderate southwest winds have formed storm slabs that have been most reactive in wind-affected terrain, or where slabs are sitting on a weak layer of surface hoar or a sun crust.
In steep sheltered terrain, small dry-loose sluffs may be reactive to human-triggering. Avoid terrain traps, such as gullies, where the consequences of a small avalanche could be serious.