Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Yesterday, skiers near Baker Ck found small, sensitive drifts in middle-elevation terrain. These slabs will be thicker and more abundant as you climb into windier, alpine terrain. Look for evidence of fresh windblown snow such as drifts, pillows, and new cornice growth. Slabs commonly form just downwind of ridgelines or on the sides of cross-loaded gullies. While I'd expect these slabs to be relatively small, they are likely to be sensitive to your weight.
Cracking, or collapsing of the snowpack are clear signs that you've found unstable snow. Given the increased chances of triggering both a wind slab and a large persistent slab avalanche on wind-loaded slopes, the prudent move is to avoid obviously wind-loaded avalanche terrain.