Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
First thing in the morning, the surface may be crunchy, and there probably won’t be much avalanche danger. That should change quickly as the surface begins to soften. Once the overnight crust breaks down, game on. Wet avalanches could go from non-existent to easy to trigger.
Pay attention to the snow surface and how it differs by aspect, slope angle, and elevation. When the surface becomes wet and heavy, it’s time to move to a different area. While it may be easy to anticipate these wet loose avalanches, determining how big they’ll get or how far they can run is tricky. They can easily grab you and drag you down the slope over cliffs or into trees.
At this point in the wet loose cycle, we’re mainly worried about human triggered slides. However, a poor overnight refreeze adds a level of uncertainty. Larger natural wet avalanches aren’t fully out of the question. These would be most likely below big rocky faces and could entrain all the snow down to the 3/25 crust. Planning routes that avoid being below these slopes helps remove the risk from these hard to predict avalanches.
(4/3/2026)
A natural wet loose avalanche near Snow Lake Divide originating in rocky terrain. Be aware of slopes above you at all times.
Photo: Craig Muderlack