Storm Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely - Very Likely
- Taille
- 1–2.5
Storm slabs are developing on top of a layer of new snow that covers the January 2 melt-freeze crust. This crust constitutes an ideal sliding plane for the upper layers of the snowpack that could lead to a natural avalanches cycle.