Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Light accumulations of new snow won’t likely tip the scales for this persistent slab problem. However, it will likely create a fresh batch of shallow reactive wind slabs in exposed terrain that could step down to persistent weak layers and become a much larger avalanche if triggered.
The likelihood of triggering one of these large avalanches that break 1-3 feet deep on buried surface hoar or facets above the 2/7 crust has gradually decreased this past week. Our last known avalanche that failed on this persistent weak layer occurred on 2/28 on Darland Mountain (observation here).
We’re getting to a point where you may or may not receive any signs of instability before triggering a large, potentially unsurvivable avalanche. Just because there are tracks on a slope, it doesn't mean it's safe. The best way you can reduce your exposure to this tricky problem is to avoid steep open slopes greater than 30 degrees, especially where the wind has formed deeper drifts, such as beneath ridgelines or in rocky terrain.
(2/28/2026)
A large, machine-triggered persistent slab avalanche on 2/28.
HS-AMu-R2-D2-O, NE, 6700'