Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Old wind slabs at middle elevations are becoming increasingly stable and are unlikely to trigger. These slabs are generally small in size in most areas. On the western half of the compass, evidence of this avalanche problem may be hard to find. The greatest concern for today is the large areas of drifted snow found primarily on east and southeast aspects. The traverse on Summer Lion Head trail is an example of an east facing slope harboring an old but large wind slab. While these slabs are continuing to gain strength, recent observations suggest that lingering instabilities persist.
To identify the avalanche problem, look for pillowy, smooth snow in east and southeast-facing terrain. Test the sensitivity by digging down to the interface of the old snow and consider potential consequences, as many of these sheltered pillowy snow drifts are harbored above exposed rocks and trees.
Summer Lion Head Traverse 2/23/24