Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 2–3
Triggering a 2-4' thick persistent slab avalanche is likely on many slopes. Persistent weak layers (sugary facets, surface hoar, or crusts) exist on most aspects and elevations. The recent storm formed or thickened slabs everywhere, and the weak layers are widespread. This means you could trigger a large, dangerous avalanche on just about any steep slope you encounter, even at lower elevations and in terrain sheltered from the wind.
Good visibility over the last few days has allowed us to observe hundreds of avalanches in the Boulder and Pioneer mountains. The avalanche cycle from the past weekend was truly remarkable (observation, observation). So far, it appears that the majority of the activity was on W-N-E facing slopes. That said, I've experienced large booming collapses on SW-S-E facing slopes over the last few days often traveling hundreds of feet and shaking snow off of trees (video).
Persistent slabs are tricky. While recently wind-loaded slopes are likely more dangerous, you can't simply look for and avoid obvious wind drifts. Nearly continuous snowpack cracking and collapsing is an obvious reminder that many slopes remain unstable. Plan your outing expecting to be able to trigger slides remotely—from gentler terrain above, below, and to the sides of steep slopes. These avalanches may break wider than expected or higher on the slope above you.
Unfortunately, avoiding slopes steep enough to slide is the only way to effectively manage this problem. Skiing or riding steep, consequential terrain is a risky roll of the dice.
(12/13/2022) Very large avalanche on a W and SW face at 10,400' at the head of Murdock Ck NE of Ketchum.