Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
At upper elevations on west through north through east-facing slopes, the snowpack’s base consists of weak, faceted snow from the early October/November storms.
This weak-faceted has now been buried under wind-drifted snow in upper-elevation terrain and capped by lingering new snow in wind-protected areas. In areas where the wind has loaded the slope, the slab could be anywhere from 2-4 feet deep and several hundred feet wide. These conditions are challenging, and while the likelihood of triggering an avalanche on this layer has decreased over the last day or two, the consequences remain just as high.
Personally, I will continue to avoid any steep northwest through north through southeast facing terrain at the upper elevations, with any steep terrain above or attached. Though this layer is getting harder to trigger, today is not the day to push it. This persistent weak layer is not going anywhere fast; the best way to handle it is to avoid it. Stick to low-angle terrain.
These types of avalanches are the ones that catch, carry, and kill the most backcountry recreationalists.