Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1.5–3
We have two persistent slab problems to consider:
- Growing Slabs Near the Surface: You could trigger a 1-2' thick slab avalanche on middle and upper elevation slopes. Snowfall over the past several days built a thin, soft slab atop weak layers of small facets or crust + facet combinations. Today's snowfall and wind will continue to grow the slab. The odds that you encounter an unstable slope increase substantially where this slab has been thickened and stiffened by the wind. Look for obvious signs of instability, like snowpack cracking or collapsing. These slides can be triggered from flat terrain—above, below, and to the sides of steep slopes.
- Thicker, Older Slabs: While unlikely, the possibility of triggering a massive 2-5' thick avalanche remains on the table. These very dense slabs also rest on weak facets and crust + facet combinations. This weak layer has been "quiet," meaning we haven't seen any recent avalanche activity or associated obvious signs of instability, but the overall poor structure (slab over weak snow) is hard to ignore. Loading during the next several days of heavy snowfall may be enough to bring this problem back to life. Smaller avalanches may generate enough force to step-down to this weak layer, producing an unsurvivable avalanche.
The combination of widespread weak snow, a developing persistent slab problem in the upper 2' of the snowpack, and the uncertainty associated with deeper weak layers should all combine to encourage conservative terrain selection. You can reduce your risk by sticking to wind-sheltered, lower angle terrain.