Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible - Likely
- Taille
- 1–2
New windslabs will form with northwesterly outflow winds. Winds slabs could overlie a weak layer of surface hoar, facets and/or a crust. Any avalanche in the upper snowpack has the potential to scrub down to these deeper weak layers, making for larger then expected avalanches. This is especially relevant at treeline elevations where surface hoar is more likely larger and better preserved.