Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–3
Since 1/31, several feet of snow has fallen on a weak snow interface, in addition to rain at lower elevations and above-freezing temperatures up to 10,000 feet. This interface is now buried beneath a slab of snow that is 2.5-4 feet thick and, if triggered, can propagate across large distances. Human-triggered avalanche activity has most notably been observed on N-NE-E aspects. With the nature of the slab of snow above this weak layer, as well as the depth of burial, apparent signs of instability, such as cracking, collapsing, or recent natural avalanche activity, are not likely to present themselves before triggering a large avalanche.
WORTH NOTING:
- Almost every change in the book has/is occurring with the current snowpack (rapid loading, wind, warming, rain...). Weird weather creates weird avalanche patterns. Lots of uncertainty exists; give steep slopes time for things to buff out.
- Activity on mid-storm snow and graupel layers has occurred, and though not a persistent layer, graupel can hang out on aprons, below cliff bands, and pop in surprising spots.
- The distribution of the 1/31 layer is variable but primarily shows its cards on the north half of the compass.
(2/3/2025)
A large skier-triggered avalanche on a NE-facing slope at 9,400' south of JHMR. It likely failed within the new snow on a density break and was thickened by wind loading. 7 skiers were caught and carried. All members of the party survived the incident.