Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–3
Yesterday (Wednesday), forecasters intentionally triggered a large, hard-slab avalanche that failed on buried weak layers in the central Whitefish range (photo above/right). This avalanche required the weight of a tumbling cornice to fail and is a reminder that it is still possible for natural or human triggers to cause a slide.
Avalanche activity on buried weak layers have been confined to aspects NW-NE-SE at mid- and upper-elevations in the Flathead Range and southern Glacier National Park. In the Whitefish Range, documented activity has been at upper elevations. Several notable weak layers have demonstrated their ability to produce large avalanches this season, including facet/crust combinations formed in late December and mid-January, as well as basal facets and depth hoar formed in November.
Here are a couple of suggestions to reduce your exposure to this hazard:
- Choose slopes with a uniform and deep snowpack
- Steer around likely trigger points, including convexities or slopes speckled with rocks
- Give cornice a wide berth and don’t linger below corniced ridges, particularly during the warmest parts of the day
- Choose lower-angle terrain
(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