Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 2–3
Skiers and riders have remotely triggered several 2-4' thick persistent slab avalanches in recent days (view Observations and Avalanches). Sun Valley Heli Ski staff observed an extensive natural avalanche cycle in the Pioneer Mtns south of the East Fork of the Big Wood River. The natural and human-triggered slides appeared to fail on persistent weak layers (crusts, crusts and facets, or facets) in the middle or bottom of the snowpack. The recent activity has been focused on slopes commonly exposed to the wind. While the slides occurred predominantly on E-NE-N aspects, triggering avalanches is possible on all aspects.
Persistent Slab avalanches can release in surprising ways. You can trigger them from flat or low-angle terrain long distances away from steep slopes, and they can break far above you. Several riders or skiers could safely ride a slope before someone triggers a slide. They can break hundreds or thousands of feet wide. Before triggering an avalanche, you may not experience snowpack collapsing or other obvious signs of instability.
Unfortunately, snowpack stability tests will not conclusively determine if a given slope will or will not produce a Persistent Slab avalanche. If your primary goal is to not get caught in an avalanche, staying off of and out from below steep slopes is the most reliable way to reduce your risk.
Observations indicate these avalanches are most likely in the southern part of this zone.
(3/4/2024) This large persistent slab avalanche failed naturally on NE-E aspects near 9000' in the Porcupine Ck drainage in the southern Pioneer Mtns. Sun Valley Heli Ski staff reported an extensive natural avalanche cycle in this area.
Photo: Sun Valley Heli Ski