Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
The surface snow on steep slopes will become wet from rain, rising temperatures, or direct sun; as it loses cohesion, wet loose snow avalanches are likely. Clear signs of of these processes include rollerballs fanning down a slope from trees, rocks, or your skis, board, or snowmachine. Move off and out from under steep slopes when and where these conditions exist. They will be most widespread on slopes getting wet for the first time, which are generally slopes above Monday's rain line (roughly 6500 to 7000 feet), or shaded mid elevation slopes.
Water percolating down below the surface can weakend and destabilize weak layers and weak interfaces, causing wet slab avalanches. These are less likely, but no less dangerous. They're also more unpredictable.
Rollerballs and debris from wet loose avalanches can trigger slab avalanches deeper in the snowpack.
(2/5/2025)
Wet loose activity on a steep and rocky southerly slope.
Photo: Flathead Avalanche Center