Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Light rainfall will gradually soften and destabilize the surface snow and increase the chance to trigger a Loose Wet avalanche. Slopes around 35 degrees, sidewalls of gullies, and areas below cliff bands are where you are more likely to encounter this problem. A superficial crust that formed over the past few days from weak freezes caps very wet snow in the middle and near the bottom of the snowpack.
As the crust breaks down, watch for rollerballs or pinwheels as clues the surface is becoming more susceptible to sluffing from added weight. As wet sluffs travel downhill, they could gouge deeper making a larger pile at the bottom of slopes or in terrain traps. The consequences of avalanche involvement are amplified by a shallow snowpack with lots of hidden or blunt objects protruding through the surface. A rotten snow surface is a clear red flag to steer toward lower-angled slopes free of overhead hazards.
(12/14/2025)
Wet Loose Avalanche Activity on an unnamed peak at the head of the Bear Creek Canyon. East Cabinet Mountains.
Photo: Jackson George