Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
What is it? A storm slab is a cohesive layer of new snow that breaks within the storm snow or at its interface with the old snow. Depending on snowfall, slabs may range from soft and harmless to thick, hard, and dangerous. This problem typically lasts a few hours to a few days.
Where is it? Storm slabs usually form in below and near treeline areas with similar snowfall, with deeper accumulations at higher elevations and in leeward terrain. Monitor storm totals to assess potential size.
What should you do about it? Watch for signs of instability like shooting cracks on small, steep test slopes. Reduce risk by waiting a day or two before entering steep terrain. If storm slabs form over a persistent weak layer (e.g., surface hoar), they may become persistent slabs, leading to longer-lasting instability.
Hot tip: Check out the Old Ski Bowl, Castle Lake or Mt Eddy snow depth sensors for new snow accumulation, helping gauge storm slab potential.