Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Winds have decreased, but isolated pockets of stubborn windslabs will likely still linger at mid and upper elevations. Avoid areas that have stiff-looking or hollow-sounding snow surfaces. If you see shooting cracks in stiff snow, you have likely found a windslab. Use small test slopes to test the sensitivity of representative slopes. When in doubt, select less consequential terrain.
Wind slabs are most likely on steep leeward slopes below cornices, ridgelines and saddles. Mid-slope features such as ridgelines/subridges can cross-load. Check out the picture below of a second natural avalanche on Pyramid. This cross-loaded pocket released naturally in a steep, rocky, and shallow snowpack area.
Carefully monitor how far you are sinking into the snow as you travel and pay attention to the stiffness and texture of the snow surface. Smooth, rounded pillow shapes, drifts, and areas of unusually deep or shallow snow are signs that wind loading has occurred. Cracking, collapsing, and strong over weak snow are signs that you have found a wind slab.
A public observation submitted 1/7/26 shows a human triggered wind slab in the Northern Wallowas.