Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 1–2
You need to continue to treat all slopes over 30 degrees as suspect. Multiple buried weak layers in the upper snowpack may not provide direct feedback to you as a traveler, but they are there and capable of producing surprising avalanches. In fact, our normal tips and tricks for evaluating stability won't work with this persistent slab problem. Uptrack tests, small test slopes, and even hand pits can't give you a sense for where or how these weak layers will fail.
With the addition of wind-loading, slabs will thicken, and our weak layers will be stressed. They could fail naturally or become primed for human-triggers. So yes - you'll want to avoid these wind-loaded areas where it's possible to trigger a wind slab avalanche. But these are the same areas where persistent grains deeper in the snowpack could result in widely breaking or remotely triggered slides.
Your best management technique will be to avoid all open slopes over 30 degrees. That includes wind-loaded terrain and even large openings in treed areas.
(2/24/2026)
A widely breaking natural avalanche in closed terrain at Crystal Mountain, in the neighboring West South zone. This one broke roughly 800 feet wide and was 2.5 feet deep, failing on the 2/13 surface hoar.
Photo: Crystal Mountain Pro Patrol