Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Moderate to strong southwest wind might develop fresh wind slabs where soft snow is available for transport.
Older wind slabs were formed by wind from the northeast and northwest. These slabs might still be reactive to human triggers, especially where they sit on feathery surface hoar.
Triggered wind slabs might step down to deeper buried weak layers and result in larger avalanches.