Wet Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 1–3
Destructive avalanches may break several feet deep on weak layers that have been further compromised by recent rain and meltwater. Runnels or rills in the snow surface indicate areas that received heavy rain. Recent avalanche activity on adjacent or similar slopes is your most obvious sign of instability.
Wet loose avalanches are still possible on very steep slopes that have not yet slid. Any slides in wet snow have the potential to step down to deeper buried weak layers. The simplest way to avoid all of these problems is to stay FAR from steep slopes until temperatures have cooled off and the snowpack refreezes.
(3/19/2026)
Slab avalanche activity in Upper Essex Creek. ( NE - 6900' ) (D 2.5). This possibly failed on a layer that was weakened by recent rain.
Photo: Michael Reavis