Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2.5
The period from 3/16-3/19 saw snowfall totals that ranged from near 3 feet at upper elevations near the coast to ~20 inches near Thompson Pass and less than a foot in the Continental zone. This new snow fell on a widespread layer of buried surface hoar, which is a variety of snow that is weak and has the potential to create instability in the upper snowpack that can persist for long periods.
Observations after 2 days of settlement have shown lots of users testing avalanche terrain in the mid elevations of Thompson Pass with no human triggered avalanches observed or reported in the last 24 hours. Steep upper elevations remain untracked in many areas. Tracks are not necessarily a sign of stability with this problem, although the amount of tracks on slopes that previously had widespread surface hoar is a good sign that this layer is stubborn to triggers along the Thompson Pass corridor. Continued assessment is advised especially when branching out into new zones.
Instability involving this layer has been reported by heli ops in the Continental zone despite lower snow totals, and in the glaciated terrain south of Thompson Pass. The sensitivity of this layer is expected to be variable dependent upon location and creates a situation where snowpack assessment can be challenging and confusing for users. Keep in mind that the terrain in the Thompson Pass area is vast and diverse. Just because you experience good stability on the buttresses of Gully 1 does not mean the same stability will exist in the Hoodoo or other areas. More observations are needed to gain a better understanding of the sensitivity of this persistent weak layer.
Human triggered avalanches remain possible that would be large enough to injure, bury or kill a person.
(3/19/2025)
Natural avalanche in the books that likely failed on 3/16 BSH
Photo: Eagan Gleasson