Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Thin slabs of wind-blown snow exist near ridges and at upper elevations in this zone. These shallow slabs likely formed over surface hoar or facets over a crust, which may make these easier to trigger. At this point, any existing slabs will be small, but they could fail easily depending on what they rest on. Look for signs of drifting and carefully consider the consequences of a small avalanche in big terrain. Steer around conseqenital slopes if you notice cracking under your feet or machine.
(3/28/2025)
Obvious signs of wind transported snow.
Photo: Dallas Glass