Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
We're only two days out from a storm that rapidly loaded a proven weak layer of facets buried in the lower third of the snowpack. A highlight reel of the recent natural activity, as well as yesterday's triggered avalanches and signs of instability, can be found in the discussion below. In summary, avalanche conditions are dangerous.
Last night's light snowfall and periods of moderate wind will keep an already stressed snowpack teetering on edge. Persistent slab problems are slow to heal. Large avalanches may be triggered in many areas, including terrain that's more sheltered from the wind. Remotely triggering slides from below, above, and to the sides of steep slopes remains a very real possibility.
Yesterday I observed a recent natural avalanche on Peak 2 in the Soldier Mountains. It was a great example of how small, thin wind slab avalanches you trigger near ridgelines could "step down", failing on layers deeper in the snowpack. You can see a quick video from yesterday here.