Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 2–3
Prominent weak layers are buried 1-3 feet deep. Snowfall and rain over the past few days has been incrementally loading the snowpack. Wind-deposited snow and precipitation will continue to load it today. It remains to be seen if this will eventually tip the balance to natural avalanches, and increase the sensitivity to human triggering.
What we do know, is that human-triggered avalanches are already possible, and as the snow piles up their potential size becomes larger. Two days ago a skier triggered a large avalanche in the Southern Bitterroot (click here for information). These same weak layers exist in the Seeley Lake region and you could expect similar avalanches anywhere you find the right slab and weak layer combination. However, it’s difficult to predict exactly where on a slope you’ll find a trigger point. As always, persistent slab problems come with inherent uncertainty.
As this avalanche problem becomes more stubborn, we’ve reached a point where we aren’t seeing signs of instability such as collapsing. So, triggering an avalanche could be the first sign of instability that you see. It is possible to remote-trigger these avalanches from below, beside, or above steep slopes. Completely avoiding this problem includes avoiding terrain threatened from above.
A portion of the crown from a large avalanche in the Seeley Zone. The full extent of this crown was 1500 feet wide. This avalanche occurred naturally on buried weak layers in a wind loaded area.
Photo: Ben VandenBos