Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2
An assortment of weak grains currently buried two to three feet deep are the perpetrators of the weak upper snowpack structure. Slopes near tree line and down to about 5,000 feet continue to be the most reactive. Fragile surface hoar grains are found primarily north and east-facing aspects. On sunnier aspects, facets above the crust are growing larger under the influence of cold temperatures, and the larger grains below are slow to heal. Even if you don't find surface hoar or a faceted crust below, places with a good helping of near-surface facets are also producing worrisome results of unstable conditions. Although the flavor of weak grains vary across aspects, these have all shown to be a problem. Due to slab depth above these persistent grains, triggering an avalanche would result in a large, potentially deadly slide.
Although all of the forecast zones have a similar set up of avalanche problem and aspect distribution, the depth of the slab on top adds variation to the potential size of avalanche you can trigger. The Selkirks and West Cabinet Mountains received higher snowfall totals from the last storm, which has resulted in a thicker slab. The Silver Valley-Bitterroot Mountains received lesser snowfall, resulting in a slightly smaller avalanche in comparison.
Photo: Izzy Davis