Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
Triggering a large avalanche 1-3 feet deep is likely above 6,500 feet on open slopes that have been exposed to the wind. 1.5-2.5 feet of snowfall over the past week buried a variety of snow surfaces, including surface hoar, near-surface facets, and crusts. This interface (buried on 2/14) has been responsible for large, natural, and human-triggered avalanches in recent days. You're most likely to encounter this problem at the middle and upper elevations, across multiple aspects ranging from W-N-SE.
Triggering an even larger 2-4 foot persistent slab avalanche on weak layers buried on 2/8 is less likely, but not entirely out of the question. This deeper, persistent slab problem exists on shaded and protected slopes at the middle and upper elevations. Slopes that remain suspect with these deeply buried weak layers face NW-N-NE.
Persistent slabs have shown the potential to propagate long distances and catch people by surprise (as shown in this photo on the right). In recent days, we've received multiple reports of people remotely triggering (from above, below, or on adjacent slopes) persistent slabs. As more time passes since the last major storm, you may not receive any clear feedback (such as cracking, collapsing, or whumpfing) before an avalanche. The weight of a snowmachine is much more likely to affect buried weak layers than a person's weight.
(2/19/2026)
This large persistent slab avalanche was triggered by a snowmobiler up Lick Creek on an east aspect, around 8,100 feet.