Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–3
Several weak layers capable of producing a large destructive avalanche can be found throughout our snowpack.
- Faceted snow formed in November near the bottom of the pack is responsible for this month's snowmobile-triggered slide in the northern Whitefish Range and the natural slide on Elk Mountain last week (Photo above/to the right).
- Faceted snow resting on the Christmas crust.
- Over the past two months, a weak layer and crust combination from mid-January has been responsible for most of the Persistent Slab avalanches. This layer is generally found 2-4 feet below the surface.
The Persistent Slab has become a low-likelihood high-consequence problem. With relatively deep snow depths across the area, these layers are generally buried at a depth that a rider is unlikely to affect. However, as recent avalanches signify, thin areas in the snowpack are likely trigger points. These include rocky outcroppings and wind-swept or scoured locations where the weak layer is closer to the surface. Last weekend riders on the east side of Glacier noted a hard slab avalanche that failed during their ascent. Mountain goats may have found one of these elusive trigger points.
Cam and Guy deliberately broke off a piece of cornice, triggering a slide on a buried weak layer Wednesday in the northern Whitefish Range (Photo above/to the right).
Terrain selection is the most straightforward way to deal with this issue. Choose slopes with a deep, uniform snowpack without a peppered rocky appearance. When in doubt, defaulting to lower-angle slopes is the best choice.
(3/22/2023)
Cornice fall triggered a Hard Slab that failed on a persistent weak layer. This avalanche occurred on a north aspect at 7100 feet.
Photo: Cam