Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Although the active wind drifting may have subsided by the time you get out there on Sunday, recently formed slabs will continue to be reactive in the right location with a human trigger. Cohesive slabs rest over the most recent (12/21) melt freeze crust, and any avalanche may propagate wider and run further than expected because of it. Look for indicators such as shooting cracks and strong over weak layering with wind drifted snow. Use test slopes to check how well recent slabs are bonding. Avoid wind exposed slopes steeper than 35 degrees if you find signs of instability or fresh avalanches. Slabs will be deeper and widest in higher elevation, wind exposed terrain, and near ridgelines. You can avoid getting avalanched by seeking out sheltered slopes and terrain less than 35 degrees in angle.
Example windslab running on a crust.