Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Weak facets and depth hoar that formed during the long dry period from November through January lurk beneath cohesive slabs that formed during the Valentine's Day storm. 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 or east at upper elevations, as well as below treeline northerly terrain where the storm snow has settled and stiffened into a cohesive slab. Expect that any slope that looks enticing enough to ride has this strong over weak snowpack structure.
Obvious signs of instability - such as cracking and collapsing - may not be present, giving 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.
An intentionally triggered avalanche on an East aspect near treeline. This avalanche was triggered from the ridgeline and failed on depth hoar near the ground.
Photo: Charlie Harrison 2/19