Storm Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
Recently formed storm slabs may not bond will to underlying layers, including weak surface hoar or facets on northerly terrain, or a hard melt-freeze crust elsewhere. Deeper deposits may be found in lee terrain features near ridges.