Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–2.5
Human-triggered avalanches breaking at the base of the snowpack remain likely. We are still within the first forty-eight hours following a peak in instability and the current persistent slab problem has shown that it gains strength very slowly following increases in natural avalanche activity. Variation in snow depth near and above the treeline has led to larger slabs with weaknesses at their margins and around trigger points in shallower areas. If triggered, the resulting avalanche could break with little warning, involving the full depth of the snowpack. Persistent slab avalanches can be triggered from below a steep slope or from adjacent slopes. These avalanches can propagate long distances and beyond terrain features that typically contain surface instabilities such as storm or wind slabs. Managing this problem is made more difficult because of our shallow and inconsistent snow coverage. The few areas with enough snow for backcountry riding are generally the same areas where the avalanche problem exists. To limit your exposure to persistent slab avalanches look for travel routes with slope angles less than 30 degrees and without overhead hazard.
(1/17/2024)
Large natural avalanche, NE aspect, 10,800', Mammoth Lakes Basin. Released overnight between 1/16/24 and 1/17/24.
Photo: Everett Phillips