Storm Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 1–1.5
Storm slabs that are somewhat small, though still large enough to ruin your day or worse, are truly touchy where they rest on large, buried surface hoar. These “slabs” are soft and barely cohesive, making it difficult to produce reliable results from our typical stability tests. Instead focus on red flag information like cracking under your feet or machine, whumphing, our 6-10” of recent snowfall, and at least some recent avalanche activity. Know that we were able to remotely trigger one such avalanche yesterday on a relatively mellow, 30-degree slope.
We expect greatest sensitivity in open areas near and below treeline, which is where you’ll likely find the largest buried surface hoar and where the wind may have added a little cohesion to our storm slab. There are also areas of near surface facets below the new snow, and some of our most sun exposed aspects have these persistent weak layers sitting on a smooth sun crust. Though fairly widespread in open areas and sparse trees, these weak layers still vary significantly on otherwise similar slopes. Some will provide instant feedback like cracking or whumphing, some will provide minimal feedback but still be capable of avalanching, and some might be stable. We’ll likely all be tiptoeing around in the mountains for a while as we watch for what these persistent weak layers produce.
(1/31/2022)
Visible surface hoar in the crown of this avalanche, a soft slab remotely triggered on a 30 degree slope, NE aspect, 6000'. Lookout Pass area.
SS-ASr-R3-D1.5-I
Photo: Ryan Matz