Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–3
In the Southeast Mountains, avalanches breaking on buried weak layers are still sensitive to human triggers in some areas. The most prominent and active weak layer is buried surface hoar a couple feet deep on the north half of the compass. There is also smaller potential for avalanches to break on faceted crust layers on some higher, southerly aspects, or depth hoar layers near the ground. Persistent slab avalanches can be remotely triggered from low-angle terrain and break larger and wider than you might expect. Lower elevation southerly aspects are generally unproblematic, and slope angles consistently less than 30 degrees are a reliable way to avoid the problem.
A broad avalanche on the north side of Crystal Peak that ran during last week's storm.