Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
At the upper elevations slab avalanches one to two feet in depth could be human triggered in steep, wind loaded avalanche starting zones. These slabs lie upon a base of faceted snow that is most developed on steep, northerly aspects above an elevation of 9,000 feet These slabs were formed by north to southwest winds and are more likely to be triggered on northerly aspects but other slopes are also suspect due to the recent loading by strong north to northwest winds.