Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
During the storm from 12/8-12/9, avalanches ran on the mid-November facets at Mission Ridge, Crystal Mountain. We suspect that a couple of observed avalanches in the East North zone also involved older weak snow layers. These avalanches ran naturally, during control work, and by skiers in backcountry terrain. Avalanches involving weak persistent snow layers are tricky and tend to stick around for a while. The snowpack will seem to adjust over time to a new snow load, then another storm rolls into the mountains, and we see avalanches breaking down onto these older layers again. Someone hitting a shallow spot near rocks or cliffs also can trigger these avalanches or large triggers such as explosives during avalanche control work. This uncertainty should make you take a step back and closely evaluate slopes that may harbor this weak snow. Steep, northerly aspects are the most suspect location for these deeply buried weak layers to exist. Be particularly suspect of steep open terrain below ridges, areas with stiff wind drifted snow, steep rolls in the middle of slopes, and near rocks or cliffs where you are more likely to trigger these avalanches. Dig down and identify sugary, faceted layers or feathery surface hoar layers buried in the snowpack. You can also use small test slopes to see if you can get a slab of snow to move. Stay on lower angle slopes if you find the overlaying snow slides easily on these layers, experience whumping collapses, or observe cracks shooting out from your equipment.
(12/10/2022)
3ft deep persistent slab avalanche in a heavily wind loaded area at Mission Ridge
Photo: Drew Carlton