Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible - Likely
- Size
- 1–2.5
Low density storm snow is expected to remain reactive to human triggers. It sits over dense wind affected surfaces and a small surface hoar layer and will take time to gain strength and bond. Expect greater slab quality and propagation in wind affected features where snow is more cohesive.
A layer of buried surface hoar or a sun crust may increase reactivity and produce larger avalanches than you expect. Reports suggest this is most prominent in the northern areas of the region around the Norns Range.