Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1.5–2.5
What is it? Triggering a large persistent slab avalanche on weak, sugary facets buried deeper in the snowpack would take some bad luck. The video to the right/above describes this problem.
Where is it? You're most likely to encounter this scenario in wind-swept alpine terrain, especially in the Pioneer, Boulder, and White Cloud Mountains. Slopes that have variable snow depths less than 2 feet deep and/or rocks poking through the snow surface are more likely spots to find this problem.
How can you recognize it? Unless you have calibrated your eyes to pick out hard, dense slabs from a distance, it is challenging to visually inspect them until you are already exposed to the avalanche terrain. Looking for rocks or bushes coming out of snow is the closest indicator to knowing the slope may harbor shallow spots to trigger these weak layers. Ethan's video is the closest visual description of how to pick this problem out from the ridgeline.
How can you manage it? The only way to effectively reduce the odds that you trigger one of these slides is to avoid alpine, wind-hardened large features on slopes steeper than about 35 degrees. Don't expect obvious signs of instability (snowpack collapsing or cracking) before a large avalanche releases. Snowpack stability tests are of little use in situations like this.