Wind SlabsNNEESESSWWNWAlta montañaLímite del bosqueBajo el límite del bosqueProbabilidadUnlikely - PossibleTamaño1–3Windslabs have formed on lees aspects and terrain features in the alpine and Treeline
Deep Persistent SlabsNNEESESSWWNWAlta montañaLímite del bosqueBajo el límite del bosqueProbabilidadUnlikely - PossibleTamaño2–4This layer could be triggered by large cornice collapses as they respond to the gradual warming trend through the weekend