West Sibillini Mountains

Wind slabs especially in gullies and bowls, and behind abrupt changes in the terrain.

The snowpack remains subject to considerable local variations. The strong wind has transported a lot of snow. In particular adjacent to ridgelines and in gullies and bowls sometimes deep wind slabs formed. In some places wind slabs are lying on a hard crust. The wind slabs represent the main danger.

Wind slabs especially in gullies and bowls, and behind abrupt changes in the terrain.

In particular in gullies and bowls, and behind abrupt changes in the terrain individual mostly small slab avalanches are possible. Avalanches can be released, mostly by large loads.