Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 3
Avalanches of previously wind-drifted snow failing on a persistent weak layer are likely on the lee side of major ridges and in and around exposed terrain features at all elevations, particularly on high slopes facing northwest through southeast.
- Slabs of wind-drifted snow formed in and around terrain features like sub-ridges, rock outcroppings, gullies, and mid-slope rollovers.
- Wind slabs of stiffer, drifted snow are rounded and smooth-looking, and they often sound hollow, like a drum.
- Beware if you cause cracking in stiffer drifted snow.
- Small loose or soft slab avalanches of new snow could overload slopes with buried persistent weak layers and cause a much larger avalanche.
- Even small avalanches can be quite dangerous if you are carried into trees or other terrain traps below.