Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1
Unstable areas of wind drifted snow likely exist on steep, upper elevation, northerly facing slopes, primarily in areas where there was pre-existing snow. The pre-existing snow has deteriorated into a layer of weak, sugary, faceted snow. This will likely turn into a persistent weak layer problem as more snow is piled on top. But for now, if you find yourself in steep, upper elevation, northerly facing terrain, avoid recent deposits of wind drifted snow. Even a small avalanche triggered in these shallow snow conditions could have devastatiing consequences.