Storm Slabs
N
NE
E
SE
S
SW
W
NW
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely - Very Likely
- Size
- 1–2
Recent storm snow and strong southerly winds have formed reactive storm slabs, particularly on lee slopes at upper treeline and alpine elevations. These slabs overlie a recent melt-freeze crust and may be easily triggered by a skier or rider.