Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 2
At the mid and upper elevations, above about 8,000’, new snow slides one to two feet deep can be triggered on steep slopes, failing on density inversions or graupel. The graupel pools below cliff bands and at the base of gullies, and on slightly lower angle slopes than you would expect.
At low elevations, below about 8,000’, you can still trigger wet loose sluffs and shallow new snow avalanches resulting in wet debris. It will take a day for all the wet snow to cool, so avoid steep slopes and especially terrain traps such as creek beds, gullies and road banks, where even a small slide can result in a deep pile of cement like debris. This includes steep, snow covered roofs at all elevations.