Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 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 upper-elevation slopes facing northwest through southeast.
- Thick slabs of wind-drifted snow formed in and around terrain features like starting zones, 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. Collapsing or whumpfing is a major indicator of instability.
- Even small avalanches can be quite dangerous if you are carried into trees or other terrain traps below.
Even a small avalanche of wind-drifted snow can have nasty consequences in certain terrain. (pc: Smoot)