Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–3
Wind slabs formed by our last storm cycle are transitioning to a persistent slab problem. Steep chutes and areas below ridgelines, on north through east facing aspects, above 5500’ were loaded with a significant amount of snow during the last storm cycle and have potential to harbor dense and stubborn slabs. While this problem is more likely to be found in the steeper terrain in the East Cabinets caution is warranted throughout the zone near these types of features as triggering a dense slab large enough to injure or bury person remains possible. Variability still exists within the zone and triggering an avalanche on deeply buried weak layers, while not likely, could have a catastrophic outcome. Evaluate individual slopes before committing to high consequence terrain.