Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Actively blowing snow and cornice formations are a great way to identify wind loaded slopes. The most suspect terrain will be steep slopes below ridgelines, confined rocky gullies, and the base of cliffs. As you travel higher into the terrain, wind slabs are likely to be larger and more easily triggered. If you identify natural avalanches, long shooting cracks, or the snow feels hollow, you should head towards low angle slopes or wind sheltered terrain.
Winds have been blowing snow around all week, and wind slabs that formed at different times will have variable reactivity. Fresh wind slabs may be very easy to trigger, but relatively small. Older wind slabs may be larger, harder to trigger, and may not show key warning signs, such as cracking. To reduce your risk, step into new terrain slowly, choose smaller slopes with lower consequences, and consider that it's probably not the day to step out into more extreme terrain.
Example photo: Wind drifted snow around features like rock outcroppings, where it's more likely you can trigger an avalanche. Note the wind transported snow visible in this photo.