Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 3
Wind drifted snow continues to be our primary concern. The most recent snow has blown into deep, dense drifts along upper elevation ridge crests, primarily on slopes facing NW-N-E. In addition, strong southerly winds have blown for more than a week drifting snow on to slopes facing W-N-SE, and we now have new wind slabs on top of old. Most of the older slabs have gained strength, but fresh drifts will continue to form in the most recent snow. Be alert to recent deposits of wind drifted snow on the lee sides of ridge crests and terrain features. Due to the intense winds, cross-loading will also be a factor so beware of the sides of gully walls and down slope sub ridges. Fresh drifts are often recognizable by their smooth, rounded appearance, and they may sound, and feel hollow underneath. Cracking in the snow surface is a sign of instability.