Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2–3
In the Northwest Mountains, there has been surprisingly little avalanche activity observed in the last week. Buried weak layers appear to have held up well to last weekend's loading event. Since early February the weak layer that produced the most avalanches was a layer of buried surface hoar and small facets, several feet deep on the north half of the compass. There is also potential for avalanches to break on faceted crust layers on some higher, southerly aspects, or depth hoar layers near the ground. Persistent slab avalanches can still be triggered after multiple people have traveled across a slope, and will be more likely to be triggered from a trigger point where the snowpack thins to a below-average depth. Avalanches breaking into old weak layers are unlikely on low elevation, southerly aspects. Slope angles consistently less than 30 degrees away from runout zones are a reliable way to avoid the problem.
A slab avalanche in Redwell Basin on the Shield. Visibility has been somewhat limited the past few days, but this avalanche represents the only evidence of recent natural activity in the Northwest Mountains.
Photo: Eric Murrow