Storm Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 3
As the snow above the persistent weak layer has become stronger and as the persistent weak layer has started to adjust to the load above it, deep slab avalanches have become more difficult to trigger and are now unlikely in most areas. In some specific areas where the weak layer remains closer to the surface, triggering one of the avalanches may remain possible. These areas could include places where a shallower overall snowpack exists or areas where trigger points like rocks, cliffy areas, single trees, stumps, etc exist on slopes with a deeper snowpack. On these slopes, several tracks could exist before a person finds the trigger point that would release the entire slope. While the possibility of triggering one of these avalanches has decreased, the consequences of these deep slabs would still be very serious.
Typical signs of instability do not usually accompany deep slabs. Often triggering a large avalanche represents the first sign of instability. Due to the uncertainty surrounding deep slab avalanches and the high consequences associated with them, making travel plans that focus on slopes where this problem is least likely to exist still represents a prudent choice. Lower angle northerly aspects still offer good recreation conditions.