Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–2.5
While persistent slab avalanches are unlikely, the uncertainty and consequences of triggering one have kept the problem on the forecast. Mountains in the central third of the zone (near and east of Mazama) would be most suspect for these avalanches. If you travel in areas near Hart's Pass, the Lost River, Eight Mile Creek, the Twisp River drainage, or the Chewuch River, be ready to make assessments of the snowpack. We know less about conditions in those areas other than they hold a weaker snowpack.
If you managed to trigger one of these avalanches, it could break widely across terrain features. Any red flag signs of danger, like shooting cracks and whumphing collapses, should be heeded. The problematic snowpack structure is a series of crusts and weak layers buried in December, now in the lower third of the snowpack. To be safe, you can choose well-supported and lower-angle slopes for travel. Stop and regroup in safer areas, well away from and out from under potential runout zones of larger slopes.
(1/12/2024)
Natural avalanches on Tamarack Peak, near Harts Pass. These likely occurred Jan 11th with northwest winds. We don't know exactly which layer these avalanches ran on, but they look suspiciously like persistent slab avalanches. E-SE, 7200ft
Photo: NCH