Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1.5–2.5
Triggering a large avalanche up to 2 feet thick is possible where weak layers have been buried since the beginning of February. The current slab sits on a variety of weak surfaces, including crusts/facets on solar aspects and facets on shady aspects. This problem could be sensitive to the weight of a single rider or snowmobile. You are most likely to trigger an avalanche on very steep rocky slopes. Specifically, consider where the overlying slab might be thin and where you can more easily impact weak layers below - such as around the margins of wind-loaded slopes. Large triggers like snowmobiles, cornices, and small avalanches in more recent snow will increase the likelihood of triggering a large avalanche. Dig down and investigate layers in the top two feet of the snowpack, but keep in mind that buried weak layers from the January dry period will be as deep as 4 feet in wind-loaded areas and will not show any signs of instability like cracking or collapsing until an avalanche is triggered. Continue to travel safely by going one at a time around steep avalanche terrain and spacing out around terrain traps like creek beds and gullies.
Additional Discussion: Small wind slabs may form at upper elevations where south winds have transported snow. Carefully evaluate terrain where wind slabs typically form, such as ridgelines, cross-loaded gullies, and leeward slopes. The formation of drifts, cornices, or blowing snow will help you identify where slopes are loading.
(2/11/2025) Photo: Bridger-Teton Avalanche Center