Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
This isn’t our typical February Wasatch setup. We have four distinct weak layers buried in the snowpack that skiers and riders continue to trigger avalanches on.
- November/December faceted snow near the ground. Particularly in rocky, shallower terrain.
- Repeater slopes—terrain that has previously avalanched.
- Late January faceted snow, present on many aspects.
- Facet/crust combos on many solar slopes. The locator rose now includes low and mid-elevation SE-facing slopes.
Avalanches may fail on a variety of weak layers, on nearly any aspect, and it’s hard to determine which one. Now is not the time to thread the needle, hoping to find the one steep slope that won’t slide—there’s just too much spatial variability.
Conditions can vary drastically over short distances, and snow pits may not reflect what’s happening nearby, even on similar aspects and elevations. Yesterday, Greg, Dave K, Dave G, and I were all out in the Central Wasatch. Each of us dug pits on some similar aspects, yet we found different layering and got different stability test results. This is a clear reminder that there’s no guarantee conditions in one spot reflect what’s happening just a few hundred feet away.
Until this snowpack simplifies, we highly recommend staying out of avalanche terrain.