Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 3
Heavy snowfall and strong winds added weight to slopes that were already near the tipping point. Very weak sugary or faceted snow is widespread across the region, and avalanches are likely where a slab of more cohesive wind drifted snow has formed on top of the weak snow.
- Avalanches failing on a buried persistent weak layer might be triggered remotely, from a distance, or worse from below!
- Cracking and collapsing of the snow are a red flag, indicating unstable snow conditions.
These large faceted snow grains make up a nasty buried persistent weak layer that is widespread in the Logan Zone. It exists on slopes at all elevations across the zone. (Beaver Mt. Backside, 2-7-2021)