Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–2.5
Old, hard slabs 2 to 3+ feet thick overlie buried weak layers and are becoming increasingly isolated and difficult to trigger. Without obvious warning signs, avalanches are most likely triggered where the slab is thinner and easier to impact the weak layer below. You can reduce your risk by avoiding steep terrain with a thin or variable snowpack, such as rocky areas, rollovers, or places where wind has created uneven slab thickness. Southerly aspects and slopes with consistently deep and uniform snow depths offer safer options.
The last persistent slab avalanche in the Northwest Mountains ran in late February on Mt. Axtell. It released below a cornice on a steep face that has avalanched multiple times this winter.