Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–1.5
Three main storm slabs exist sandwiched between rime crusts sitting on top of our very firm base of various melt forms. There is a high amount of variability of depth of storm slabs and existence of rime crusts. While the structure of the snowpack has the potential for slab avalanches, unreactive stability tests, lack of a temperature gradient, and no recent signs of instability lead to slab avalanches being unlikely and relatively small in size.