Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 1–2
Snowfall and wind drifting in early December formed slabs up to a few feet thick over facets near the ground. These weak layers are most widespread on the northern half of the compass. Mild weather through the middle of December has helped the snowpack adjust to its current load, or in some cases, the shallow snowpack has seen slabs completely facet away. A recent extreme wind event has further wind-hardened or wind-eroded many exposed slopes. Identifying where the most likely areas to trigger this old avalanche problem are currently difficult. Obvious signs of instability and strong over-week layering in the snowpack are two potential red flags. Continuing to use good travel techniques in avalanche terrain will also help reduce your group's exposure to this avalanche problem.
An old persistent slab avalanche that was triggered on the east side of Cinnimon Mountain. 12/14.