Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Unlikely
- Dimensione
- 2–3
New and wind-drifted snow has added a modest load to buried weak layers. Previous unassuming loading events still produced isolated natural avalanches large enough to destroy a wood frame house. Slides failing on weak layers have been confined to aspects NW-NE-SE this season.
Weak layers are generally buried at a depth that a rider is unlikely to affect, but thin spots in the snowpack remain potential trigger points for backcountry riders. This concept is supported by last week's - potentially goat triggered - avalanche on Red Crow Mountain, just outside the advisory area (Photo above/right). Small surface slides or cornices have more mass than a human or machine and can still affect buried weak layers even where the snowpack is deepest. On Wednesday, Cam and Guy deliberately broke off a piece of cornice, triggering a slide on a buried weak layer in the central Whitefish Range.
Use one or more of the following methods 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
- Choose simple or lower angle terrain
(3/22/2023)
The crown of a hard slab avalanche that may have been triggered by goats in southern Glacier Park, east of Marias Pass. This crown has been partially filled in from wind-loading.
Photo: Tyler Lucas