Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 1–2.5
Up to two feet of new snow and wind drifting have formed easily triggered slabs that will be most sensitive on wind loaded slopes at higher elevations or on the north half of the compass where they are forming over fragile weak layers. Storm slabs can be remotely triggered from below steep slopes because they formed on surface hoar. Instabilities in the upper snowpack have the potential to step down and trigger larger and more dangerous persistent slabs where the problems overlap. Stay off and out from underneath slopes steeper than 30 degrees to avoid the problem.
2/4: A 12" storm slab triggered yesterday at the Anthracites. Slabs are twice as thick today in some parts of the Northwest Mountains.