Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 4
There is a persistent weak layer (PWL) of faceted snow buried on most slopes except ones facing south and southwest. Most steep slopes have avalanched at least once if not multiple times, and the layers left behind are quite variable but still capable of producing a slab avalanche.
Yesterday while riding through a large chunk of the Uintas, my group experienced many collapses especially in rocky areas. Collapses are an obvious sign of instability we can't ignore. At the same time, we didn't see or hear about any recent slides. Craig got an overhead view of the Uintas yesterday and didn't spot any recent slides either. However, the skier triggered slide in the Wasatch Range, which generally has a stronger snowpack, is a good warning sign.
What does all this mean? The odds of triggering a slide on a PWL have gone down a lot, but they are not zero. If you choose to enter avalanche terrain and ride steep slopes, stack the odds in your favor. Avoid areas of thinner snow near rocks (sometimes hard to do), make sure the runout zone is free of trauma-inducing trees and rocks, and make sure your partners watch you from a safe area.