Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Recent winds formed wind slabs along ridgelines and alpine terrain features at mid and upper elevations. We expect most wind slabs to be small, but there's a chance they could step down to deeper weak layers or break wider than anticipated. If you see cracks shooting away from your equipment or hear whumping collapses, avoid steep wind-loaded slopes below ridgelines, the base of cliffs, and cross-loaded terrain features. Textured surfaces and visible blowing snow are great visual clues to identify wind-affected terrain.
With the variability in the old snow surfaces, this problem could be tricky to pin down, and similar slopes may not react the same. With increased uncertainty, build in greater margins of safety and step into new terrain slowly, making frequent assessments before committing to steep slopes. An avalanche on an east aspect of Snagtooth ridge that propagated into older, deeper snow layers highlights our complex and variable snowpack. (See video) This could be an isolated incident, but it's probably best to keep it in mind when choosing terrain. Consider avoiding shallow, weak areas in the snowpack, typically found in or near steep, rocky terrain.