Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Wind slab avalanches will be most likely where slabs have built up on weak near surface facets that developed prior to the start of the latest storm. In the right terrain, wind slabs will have the ability to propagate faster and further than what we typically see. Wind slabs will be of greatest concern in shaded and cold N and NE facing terrain. On some slopes wind slabs will be stubborn and non-reactive. Wind slabs form in specifc places and are typically below ridge tops, high points, and around features that catch blowing snow.