Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Our persistent weak layer (PWL) continues to plague us, with direct and remotely-triggered avalanches 2-3 feet deep and up to 200 feet wide occurring almost daily:
- Sunday - Butler Basin skier-triggered on north aspect at 9,200'. Rider caught and carried.
- Tuesday - High Ivory remotely-triggered on east aspect at 10,000'
- Wednesday - Hallway Couloir remotely-triggered on northwest aspect at 10,400'
- Thursday - Pioneer Ridge skier-triggered on north aspect at 10,100'. Rider caught and carried. (photo below)
You can find the PWL at the mid and upper elevations on aspects facing west, north, and east (see the locator rose above). Most of the avalanches failing on the PWL are occurring in thinner snowpack areas (such as steep, rocky terrain) where it is easier to trigger the avalanche where it then propagates widely to areas where the snowpack is deeper. Signs of instability - such as cracking and collapsing - are now uncommon and existing tracks on the slope are no indication of stability.
The easiest way to handle this problem is avoid slopes steeper than 30° where this problem exists.
On Thursday, Russ Costa and I traveled to the UFO Bowls in the Provo mountains where we found a shallow snowpack with poor structure. In the video below, I describe how we handled this situation.