Prags Dolomites

Weak layers in the old snowpack represent the main danger.

Weak layers in the old snowpack represent the main danger.

In some places avalanches can be triggered in the weakly bonded old snow, in particular on very steep west, north and east facing slopes above approximately 2200 m, as well as on very steep sunny slopes at elevated altitudes. Avalanches can in isolated cases reach medium size. As a consequence of a strong to storm force wind from northwesterly directions, mostly small wind slabs formed. They are to be evaluated with care and prudence in steep terrain. Caution is to be exercised adjacent to ridgelines and in pass areas, as well as at elevated altitudes. As a consequence of warming during the day and solar radiation individual gliding avalanches and moist snow slides are possible, but they will be mostly small.

Towards its base, the snowpack is faceted and weak, especially on steep west, north and east facing slopes above approximately 2200 m, as well as on steep sunny slopes at elevated altitudes. The fresh wind slabs are lying on weak layers in particular on shady slopes above approximately 2400 m. A little snow is lying.

Weakly bonded old snow requires caution.