Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Widespread layers of weak snow can produce large avalanches here. These are buried beneath dense, 1-4 plus foot thick slabs, which makes triggering slides more difficult. These thick slabs also mean that any slide you trigger will be large and destructive. Do not expect feedback to receive obvious feedback from the snowpack today. The first sign of instability may be the large, wide avalanche that you trigger. These slides can be triggered after dozens of skiers or riders have traversed a slope. Triggered slides are likely to break far above you, making escape difficult to impossible.
Avalanche activity during major storms in March was widespread, occurring on all aspects. Many huge slides in this zone failed on persistent weak layers in the upper and middle portion of the snowpack. You'll find a variety of weak layers here (crusts with facets on solar slopes, and facets without crusts on shaded slopes). As meltwater percolates through the snowpack it can weaken the bonds underneath dense slab, producing large wet slab avalanches. Similar conditions at the end of January produced a widespread cycle of wet slab avalanche activity. Most of the slides observed then were large enough to destroy your house.
Triggering a slide is most likely in steep, rocky, open, heavily wind-affected terrain (photo at right/above). You can reduce your risk by avoiding this type of terrain.
(3/6/2024) Very large avalanche on a SE aspect above Window Lake north of Boulder Basin. Photo: Sun Valley Heli Ski