Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 3
Most natural avalanches in the Logan Zone occur during windy winter storms. Heavy snowfall and westerly winds today will add weight and overload slopes with poor snow structure that are currently near the tipping point. Buried persistent weak layers consisting of sugary faceted snow are widespread across the Logan Zone, and the threat of large and deadly avalanches failing on weak snow near the ground remains quite real.
- 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.