Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
You'll find deep drifts as you gain elevation, especially in the Wenatchee Mountains, Salmon la Sac, Teanaway, and Icicle. These slabs are likely to be resting over weak, faceted surfaces or the slick Early February Crust (EFC). To avoid triggering an avalanche, stick to lower angle and well supported slopes at mid and upper elevations. You can expect to find slabs below corniced ridges, convex rolls, steep gullies, and at the base of cliffs. Look and feel for pillow-like drifts and similar wind textured surfaces to clue you into this potential. Its mid February, and the suns stronger rays may create cohesive slabs even outside of wind drifted areas. This is a somewhat unique setup where you might be able to trigger slab avalanches on south facing slopes by mid day because of this. On Tuesday, skiers in the Icicle Creek area triggered a small wind slab that failed on weak, faceted snow over the EFC. While this avalanche was small, it may be a sign that we could begin to see large or surprising avalanches failing on persistent weak layers with this additional snow load.
(2/13/2024)
Skier triggered wind slab on the early February Crust on a NE aspect at 6,500ft in adjacent Stevens Pass on Tuesday.