Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
This isn’t our typical February Wasatch setup. The snowpack holds four distinct weak layers, all of which continue to produce skier- and rider-triggered avalanches:
- November/December facets near the ground, especially in rocky, shallow terrain.
- Repeater slopes—areas that have previously avalanched.
- Late January facets, found on many aspects.
- Facet/crust combos on solar slopes, now extending into low- and mid-elevation SE-facing terrain.
This snowpack is anything but straightforward. Avalanches can fail on multiple weak layers, on nearly any aspect, and there’s no clear way to predict which one will go. Now is not the time to try and thread the needle, hoping to find the one steep slope that won’t slide—there’s just too much spatial variability.
Conditions can change drastically over short distances, and snow pits may not accurately reflect what’s happening nearby, even on similar aspects and elevations. Stability in one spot doesn’t guarantee the same conditions just a few hundred feet away.
Until this snowpack becomes more predictable, we strongly recommend staying out of avalanche terrain. Any avalanche in the new or wind-drifted snow has the potential to step down into one of the deeper persistent weak layers.