Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
Triggering a large 1-2 foot thick avalanche on a buried weak layer is today's primary problem. This is more likely where the wind stiffened the surface snow into a cohesive slab. Suspect slopes include those with signs of wind effect, such as pillows, dunes, and etched surfaces. Buried weak layers (facets, faceted crusts, and surface hoar) are found on many slopes at all elevations and rest beneath February's snowfall.
Slopes that will be easier to trigger will be steep (35+ degrees) or associated with a convexity or rollover. Since the weak layers are not buried deeply, they should be sensitive to the weight of a rider in many locations. In deeper drifted areas, avalanches will be easier to trigger in thin spots at the edges or where rocks stick out of the snow.
Observers in the southern Whitefish Range have noted signs of instability like collapsing (whumpfing), shooting cracks, and a triggered avalanche over the past few days. We suspect this could or is occurring in other zones as well. These signs are red flags directing you to lower-angle terrain free of overhead hazards. Thursday's avalanche (Attached image) confirms you can trigger avalanches remotely—from flat terrain below, above, and to the sides of steep slopes.
(2/15/2025)
This image shows the skin track and approximate location where a remotely triggered hard slab avalanche occurred on 2/13/25. The slope angle varied between 30 degrees at the trigger point to 40 degrees at the crown.
Photo: Mark Dundas