Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 1–2
A widespread and firm surface crust is making it difficult to influence persistent weak layers that are buried 2 to 3+ feet deep. While the snowpack structure is still present, these weak layers have shown that sensitivity is decreasing and stability is trending in a positive direction. Minor differences across the forecast zones exist; the January 1st buried surface hoar has been more present in the Northern Mountains but has been more difficult to find in the Silver Valley-Bitterroots as a result of the brief January 2nd- 3rd rain event that climbed higher in elevation in the south, which helped destroy the surface hoar in many areas.
While the sensitivity of these weak layers has trended towards unreactive, the places you might still be able to trigger a large avalanche are found in isolated areas where the snowpack has a soft surface and is shallower in steep, rocky complex terrain. If you choose to travel in this type of terrain, avoid complacency and continue to use safe travel habits.
A large natural avalanche that was probably triggered by rapidly warming temperatures following an extended period of cold, snowy weather. The slide failed on a northeast aspect around 5,350 feet, and we estimated the crown around 4 feet deep, likely failing on a buried persistent weak layer.
Selkirk Mountains. January 14, 2026.
Photo: Chris Bilbrey