Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2–3
It is still possible for a rider to trigger a large avalanche that breaks 1 to 4 feet deep on steep slopes. Audible collapses were observed in all three zones during the past week and as recently as yesterday (Wednesday). Whumpfing collapses are a clear sign that buried weak layers remain sensitive to the weight of a person or machine. The problematic structure - weak facets over a hard crust - appears most developed on slopes facing east through south to west and areas close to the Continental Divide. At low elevations, this hazard exists on roadcuts and other steep slopes with continuous snow cover.
The most reliable way to reduce your exposure to this hazard is by staying off of and out from under steep slopes. In the absence of clear signs of instability—like recent avalanches, or collapses—do your due diligence by digging into the snow and looking for faceted, “sugary” snow near a crust 1 to 4 feet below the surface. Riding a slope where you find this layer includes the risk of triggering a potentially deadly slide.
(1/24/2024)
Observing the crown of a natural D2 slab avalanche. This slab failed on weak snow above the 12/22 crust and likely ran Sunday 1/21.