Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1.5–2.5
Weak layers of faceted snow that formed in November sit below recently formed slabs and are under considerable stress from recent loading. These slabs are generally 2-3 feet thick and could be hard or soft depending on location. This problem is confined to upper elevation terrain and shaded aspects at the mid elevations. East through north facing slopes held the most continuous and well developed weak snow prior to the recent storms. While the likelihood of triggering is slowly decreasing, there is still a good chance that a human can trigger a large persistent slab avalanche in very steep (>35deg) upper elevation terrain. Wind loaded slopes will produce the largest and most destructive avalanches. It is likely that obvious signs of instability, such as cracking or collapsing, will not be present prior to triggering.
A large explosive triggered hard slab at JHMR. This avalanche is about 3 feet deep and failed on faceted grains above a melt freeze crust -(12/8/2025)