Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Recent storms have dumped over a foot of new snow since Valentine's Day, which is starting to form a cohesive slab. This problem has been observed on a large variety of aspects and elevations, and will likely be more obvious at upper elevations where the wind has accelerated slab formation. Cracking around your skis, machine, or in the corners of your skintrack is a sign a slab has formed. Hand shears and small test slopes are excellent tools to help identify this problem. Carefully monitor the size and depth of these slabs as they continue to settle, and avoid terrain where you find more than 4" of cohesive snow on the surface.
(2/18/2026)
A shooting crack in sheltered terrain around 7000'.
Photo: Sarah Jakober