Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1–2
Stability around the recent storm snow interface (12/8) seems to be improving. However, there is still potential to trigger an avalanche on this layer. Unlike a typical storm snow interface, the new snow fell on weak, persistent grains that take a while to strengthen and heal. Over the weekend, reports came in with skier triggered avalanches on this layer, and Crystal Ski Patrol triggered an avalanche on a 3-4ft deep weak layer that was formed and buried in November. We have limited direct observations from the East South zone. However, similar snowpack and avalanche conditions likely exist in East South. We have significant uncertainty about the distribution and reactivity of these weak layers, so assessing the snowpack is essential before committing to steep slopes. Approach new terrain slowly and assess conditions as you ascend in elevation. Steep, northerly aspects are the most suspect location for these deeply buried weak layers to exist. Weak layers buried by the recent storm may be more widespread. Be particularly suspect of sparsely vegetated slopes, steep open terrain below ridges, steep rolls in the middle of slopes, and near rocks or cliffs where you are more likely to trigger these avalanches. Dig down and identify sugary, faceted layers or feathery surface hoar layers buried in the snowpack. You can also use small test slopes to see if you can get a slab of snow to move. Stay on lower angle slopes if you find the overlaying snow slides easily on these layers, experience whumping collapses, or observe cracks shooting out from your equipment.
(12/10/2022)
A distant view of the skier-triggered avalanche at White Pass on 12/10. This slide is suspected to have failed on buried surface hoar.
Photo: Paul Przybylowicz