Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Very Likely
- Dimensione
- 1–2
The higher in elevation you travel, the more likely it will be to find terrain that a wind slab will have formed in. But with strong wind speeds, you could encounter wind affected snow lower down on slopes than you might expect. With shifty wind directions throughout the week, older and largely unreactive slabs may exist on a wide variety of slopes, but deeper and fresher slabs will probably be found mostly on north and east facing terrain. The likelihood of triggering a large avalanche is lower in areas further east, such as the Wenatchees.
Wind slabs typically form just below ridgelines and in gully or chute-shaped terrain features. Look for clear signs of wind transport: dune-like drifts, cornice formation, and blowing snow. As you move about the terrain and the snow underneath you begins to feel denser and look unevenly distributed, assume wind slabs probably lurk nearby. In addition to cracking and collapsing, recent natural slab avalanches are very good reasons to avoid exposed terrain steeper than 35 degrees.
If you plan to travel to upper elevation terrain close to the Crest, stick to sheltered terrain less than 35 degrees. Lower down, approach steep, unsupported terrain with some suspicion, as storm slab instabilities may also exist. You can push around in a simple hand pit or on an inconsequential test slope to help gauge the reactivity of the recent storm snow.
(3/18/2025)
A small sledder triggered wind slab avalanche in the Salmon La Sac last weekend. SS-AMu-R1-D1-O
Photo: Evan Pearson