Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 1–2.5
Rain on snow will cause widespread avalanching. Expect to see this on roadcuts and some lower elevation terrain that may not slide often.
Wet loose avalanches typically start in terrain steeper than 35 degrees, and while they travel slowly, they are very dense/destructive and can travel long distances into the flats.
With this volume of rain, Wet Slab avalanches are possible if liquid water percolates down to a crust or bed surface.
(1/12/2025)
An example of an avalanche runout zone in the Northern Wallowas
Photo: Steve D