Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Rain seeping down into the snowpack can weaken the bonds at the interfaces between layers causing wet slab avalanches. Notable layer boundaries in the upper and mid snowpack are the Dec. 16 crust down 8-12", and Dec. 9 crust down almost 2 ft. If these interfaces become wet and weaken/fail, the layer(s) above can slide and the resulting avalanches could be large.