Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–2
A mix of facets and faceted crusts buried 1 to 3 feet deep continues to produce large human and remote-triggered avalanches in the adjacent Northwest Mountains, and additional loading today could cause the problem to become more common in the Southeast Mountains. Northerly and easterly facing terrain near and above treeline has been most active due to thicker slabs over well-developed weak layers. The lower half of the snowpack is highly variable, shaped by early-season droughts, record-warm temperatures, rain, and past extreme wind events. As a result, expect inconsistent feedback as you move across aspects, elevations, or even different parts of the same slope. Obvious signs of instability may be absent, and the first clear signal could be a dangerous avalanche. The most reliable way to manage this problem is by choosing slopes less than 30 degrees. Wind-eroded terrain, sunnier aspects, and lower elevations generally offer lower risk options, where slabs are less common and weak layers are often capped by thick crusts.
A large, remotely triggered avalanche on Schuylkill Ridge on Sunday.(1/4/2026) Photo: Crested Butte Avalanche Center