Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
This avalanche problem is becoming increasingly scary as the problematic weak layers of old faceted (sugary) snow (Dec 11 PWL and Dec 17 weak layer) are buried deeper in the snowpack. The weak layer(s) associated with this avalanche problem have reactivated under the new snow load. One of yesterday's avalanche incidents appears to have been a persistent slab avalanche. This avalanche problem exists on W-NW-N-NE-E aspects, has a widespread distribution in below treeline and near treeline terrain, and isolated distribution above treeline.
Whumpfing, shooting cracks, recent avalanches, and unstable snowpit test results are all indications of unstable snow in the area. Do not write off the significance of any of these clues when dealing with a persistent slab avalanche problem, even if they seem isolated. If you choose not to scale back route choices to less than 30 degree angle slopes only, this is a difficult avalanche problem to manage. Signs of instability may or may not readily present themselves prior to triggering an avalanche. Do not underestimate potential avalanche size, potential runout distance, or the hazard from connected terrain above or to the side. It would be fairly easy to encounter a persistent slab avalanche today while trying to avoid wind slabs. Route find to avoid both.
Weak layer unverified but the jagged crown suggests a persistent slab avalanche. Skier triggered on the ascent from the red X location on Nipple Pk.