Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Slab avalanches may be easier to trigger in the morning as an overnight storm wraps up. After a generally warm Friday, temperatures should start to drop, which could result in lower-density snow on the surface. While this snow could fail in slabs or loose, you'll also need to look for deeper layers from the past several days as potential weak points in the upper snowpack. The rising and falling temperatures mean a new crust could exist below Friday night's storm snow, creating an excellent bed surface for avalanches to run on. Springtime weather has delivered periods of graupel, which can act as a short-lived weak layer. Use uptrack tests, small test slopes, and quick hand pits to gauge the upper snowpack's slab potential. If blocks fail easily in your tests, you find a poor bond at the new/old interface, or discover an upside-down snowpack (heavy snow over weaker snow), then you should avoid slopes over 35 degrees where triggering a slab is more likely.
Slabs will be larger and possibly more reactive on the volcanoes or wind-affected terrain.
(3/21/2025)
A slab avalanche in Pickhandle Basin near Crystal Mountain. This one looks to be in wind-loaded terrain.
Photo: Dallas Glass