Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
Weak facets and depth hoar that formed during the long dry period from November through January are capped beneath cohesive slabs from last Tuesday's storm and the strong winds yesterday. These widespread weak layers are 1 to 3 feet below the surface and remain easy to impact in travels. The most dangerous slopes face north and some east, mainly at upper elevations but also extend to below treeline in more open northerly facing terrain where winds have helped build cohesive slabs. Expect that any slope that looks enticing enough to ride has this strong over weak snowpack structure.
Obvious signs of instability, like cracking and collapsing, may not be present and give you a false sense of security. It's still possible to trigger an avalanche remotely from the flats below or on an adjacent slope. Any avalanche triggered has the potential to take with it most of the season's snowpack and be large enough to injure or bury you.
Depth hoar, facets and faceted crusts remain weak and will continue to be stressed by loading from yesterdays strong winds.
(3/5/2025) Photo: Andy Bond