Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 1–2
Basal facets buried at the bottom of the snowpack continue to persist on northern facing slopes in a few locations. In general, these facets seem to be nearly gone, except in rocky and talus bed surfaces. Over the last week to two weeks, they have been unreactive in stability tests, including those conducted in pits averaging just 50 cm. Nonetheless, skiers and riders should continue to exercise caution in the starting zones of steep chutes. The variable conditions across terrain make this problem difficult to assess, and it is possible that some slopes still harbor reactive layers near and at the bottom of the snowpack. The only way to fully know if this persistent weak layer is still present and possibly reactivity is to dig. Given the mostly rocky bed surface strewn across the San Francisco Peaks; this problem could still produce a small to large avalanche capable of burying a skier or rider.