Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2
Wind drifts and storm slab avalanches may be triggered in localized terrain, primarily in the mid and upper elevations. The snow structure is generally capped by recent rime and freezing rain. We'll need to keep an eye on this structure to watch for any development of weak faceted snow beneath the crusts that may affect avalanche conditions in the future.