Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 3
Avalanches of wind-drifted snow are likely in and around exposed terrain features in upper elevation terrain, particularly on northerly facing slopes.
- Slabs of wind-drifted new snow will form 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. Shooting cracks and whumpfing are obvious signs of instability.
- Avalanches could be triggered remotely, (from a distance or from below)