Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2.5
The period from 3/16-3/19 saw snowfall totals that ranged from nearly 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 weak snow that has the potential to create instability in the upper snowpack that can persist for long periods.
After 3 days of observation, the sensitivity and distribution of this weak layer is coming into better focus. The snowpack along the Thompson Pass road corridor has not shown signs that a reactive weak layer is present. In tact buried surface hoar has not been identified in snowpits in terrain that drains to the road. Expect buried surface hoar to remain reactive in isolated pockets of steep terrain near Thompson Pass.
Reports of identifiable buried surface hoar in snowpits and human triggered avalanches have come from glaciated valleys that are colder and more protected than the core Thompson Pass area. Instability is expected to be more prevalent in these areas. Don't assume that the same snowpack structure and stability exists in all areas. Continued assessment is advised especially when branching out into new zones.
The sensitivity of this layer is expected to be variable depending on location creating 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 in the Thompson Pass road corridor does not mean the same stability will exist in more remote zones. 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