Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Overall, signs of instability have decreased as the snowpack continues to settle, though active winds persist above treeline. While many surfaces lack the distribution of a congruent slab through the terrain, smaller pockets of wind drifted snow remain possible to trigger.
Erratic north and northeast winds have been transporting snow over ridgelines, around rock outcroppings, and across open slopes. Although wind speeds are near the upper threshold for slab formation, incremental loading in isolated areas could catch an unsuspecting rider off guard. Clue into the snowpack and terrain: where is snow blowing, which surfaces appear wind-textured or lens-shaped, and does cracking occur on small test slopes. These observations can help you identify terrain features worth avoiding.
(12/28/2025)
Active wind loading in upper Avalanche Gulch
Photo: Hayden MacArthur