Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Wind slabs could exist in more exposed locations along ridgelines, in gullies, around rocky outcroppings and other features on exposed mid to upper elevation terrain. Unusual wind directions shifted snow into areas that don't normally collect deposits. Subtle drifting formed soft slabs, ones that aren't as hard as what we sometimes think of with wind slabs. These unusual softer slabs may be more tricky to identify. They may not be large enough to bury you, but if you're in high consequence terrain they could still cause harm.
Pay attention to changes in snow texture and depth as you gain elevation and change aspects. These changes could happen quickly, where you might find major differences in only a matter of a couple feet. Signs of recent wind-effect like scoured snow surfaces and drifting behind features are good indicators of where you might encounter additional deposits. Hand pits and test slopes can help you gauge the bond of wind slabs, but don't ignore obvious signs of instability like whumphs, shooting cracks, and recent avalanches. If you encounter these signs of instability or see clues of drifting, avoid nearby slopes that are greater than 35 degrees.
This is a good visual for locations of possible wind slabs. Photo: Dallas Glass