Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
Snow and wind-loading in the past week have formed a new generation of slabs up to several feet thick over small-grained facets in the upper snowpack. Numerous natural and triggered slabs have occurred on this layer in the past few days. Slabs are larger and most sensitive near and above treeline on wind-loaded slopes, especially on colder aspects. Give leeward terrain a cautious buffer by choosing lower slope angles or smaller terrain features, while staying alert for potential instabilities on wind-sheltered terrain.
On unusually shallow slopes, most commonly in the Southeast Mountains, there is still a small potential to trigger a destructive avalanche that breaks on deeper weak layers. The most concerning structures are on northerly aspects near and above treeline where snow depths are less than 170 cm.