Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1.5–2.5
Dropping freezing levels overnight and refreezing surfaces are slowly reducing the likelihood of triggering wet avalanches. However, there is still plenty of rain and meltwater swimming around in the snowpack. Until that water drains out or the snowpack fully refreezes, there is still some chance of encountering a large avalanche. Sagging cornices are also highly suspect, as one of these big chunks of snow could detach without warning. These aren’t problems you can evaluate with regular snowpack observations, and it’s unlikely you would trigger one. The only real way to reduce your risk is to limit the time spent on slopes steeper than 35 degrees, as well as just below cliffed and corniced ridgelines.
Small amounts of new snow at upper elevations will be easily influenced by sun and warm temperatures. If you get high enough to find freshly fallen snow and its getting moist and sticky, note that triggering very small wet loose avalanches will become easier. These won't bury you, but could knock you off your feet and carry you into terrain traps below so be cognizant of your terrain selection as you travel around. A thin, superficial surface crust may exist on the surface in the morning, limiting this problem, but it will break down as the day heats up.
(1/14/2026)
An example of wet slab avalanche crowns from earlier in the season. Spire Gully, Hairpin Valley, NE, 7,000ft
Photo: Josh Hirshberg