Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Faceted weak layers from December deeper down in the snowpack continue to persist on N through E and SE aspects near and above treeline. These weak layers are lingering typically in the bottom 60 cm of the snowpack with the January and February storm snow forming slabs on top of these weak layers. Triggering one of these deeper weak layers may take finding the right slab/weak layer combination or where the overlying slab is thinner and weak layers are shallower. It may not be the first, second, but may take the fifth person on a slope to find a "sweet spot" to get the slope to avalanche.
Avoid likely trigger points, near rock outcrops, steep convex rolls, and on the margins of the slab. Obvious signs of instability like shooting cracks and loud audible collapses most likely will not be present in travels and lure you into steeper terrain. Using a probe pole to feel for strong over weak layering or taking the time to dig down into the snowpack is a great way to assess if this poor snowpack structure exists. Any persistent slab avalanche would be large and dangerous potentially taking with it most of the season's snowpack. Giving avalanche paths wide berths, avoiding being on or connected to slopes over 35 degrees is a great way to stay safe.
Faceted weak layers and depth hoar that formed earlier in the season continues to linger deeper down in the snowpack beneath stronger cohesive slabs.