Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Upon finding facets and poor structure on multiple E-S-W aspects Tuesday, we've expanded the distribution of this problem to southerlies. Below 4000', there is not enough of a slab overlying the persistent weak layer (PWL) to warrant listing.
The thickness of the overlying slab varies from 1-1.5' (or more with wind loading). The persistent weak layer below can be summarized:
- On shady and wind-sheltered northerly aspects, February's snow has not bonded well to the 10-12" of weak, sugary facets and/or surface hoar.
- On solar aspects, a buried melt-freeze crust may provide a slick bed surface and harbors weak sugary snow below it. We have had one confirmation from the S Wallowas of a persistent slab triggering below the 1/31 melt-freeze crust.