Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 1.5–2.5
The odds of triggering a slab avalanche on weak layers buried 1 to 3 feet deep continue to decrease. The weak faceted snow responsible for a rash of avalanches between January 7 and 14 is slowly gaining strength.
Unfortunately, we don't know which slopes have a slab-weak layer-crust setup, responsible for the Persistent Slab problem. Instead, consider the snow surface you travel on. Slopes with a supportable surface crust are found on sunny aspects and are generally the safest, as they limit the stress you place on the weak layer. Shady areas harbor a thin, weak crust, or none at all, allowing your weight to impact deeper into the snowpack, potentially triggering a slide.
With the current poor-quality surface snow, choose a low-angle slope where you have a better chance of both controlling your speed and avoiding triggering a large avalanche.
This problem is challenging because the usual signs of an unstable snowpack, such as cracking or collapsing, are often absent before triggering a slide. If you decide to ride a steep slope, choose a runout free from terrain traps such as trees, gullies, and cliff bands to improve your odds if something goes wrong.
(1/11/2026)
This small avalanche was remotely triggered by riders in the sidecountry east of WMR. This likely failed on weak snow above the Christmas Crust. Although unlikely, riders can still trigger a slide similar to this.