Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
Most slopes currently have very weak and fragile facets and depth hoar on or near the ground that formed during the prolonged November and December dry periods. Recent snow and wind loading have built cohesive slabs on top of these persistent weak layers leading to this poor snowpack structure of strong over weak. These weak layers haven't received much of a break and will need more time to adjust to the loading we've seen over the last week. These persistent slab avalanches can break widely across the slope or terrain features and could be large taking with it most of the season's snowpack and most likely would not be survivable. You can trigger one of these large avalanches from a long distance away, so continue to give steep slopes above you wide berths.