Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Unlikely
- Taille
- 1.5–2.5
Poor snowpack structure exists on shaded aspects where weak snow exists two to four feet beneath a hard slab. The weak layers are now capped by a stout rain and temperature crust up to 9,500’ and firmer, settled snow above that elevation. These firm to hard slabs lie two to five feet above weak layers that appear to have become unreactive to triggering. Though stability test pits show moderately unstable results, you could make a good case that these results are false given that other signs of instability like cracking, collapsing and avalanches are not currently present. That said, slope failure cannot be ruled out entirely in isolated areas above about 9,500’ where wind has redistributed snow and possibly brought the weak layer within reach of triggering. This avalanche problem will be tested again in the next few days as a new load of snow is applied.
(12/11/2025)
Large natural avalanche that occurred at the end of the storm on Dec 10th. Slab formed by wind loading looks to have failed on the persitent weak layer buried in early November.