Avalanche danger above 2200m is moderate, below that altitude danger is low. In few places, an avalanche can be triggered by one sole skier as a slab avalanche. Danger zones are nearly impossible to recognize, most critical behind protruberances in the landscape and in gullies and bowls. Fresh drifts on some ridgeline slopes can be easily triggered as a small slab. The wind-loaded zones are easily recognized, watch out for the risks of falling. On very steep sunny slopes, small loose-snow avalanches are possible. Isolated small naturally triggered glide-snow avalanches are possible.
Snowpack
Atop a hardened crust (or else, bare ground) 10-30 cm of loosely-packed snow lie deposited, often wind impacted. On shady slopes at high altitudes the fresh snow from Friday has also been deposited atop loose snow or surface hoar. The fundament on steep shady slopes at high altitudes is expansively metamorphosed. Atop a hardened crust (or else, bare ground) 10-30 cm of loosely-packed snow lie deposited, often wind impacted. On shady slopes at high altitudes the fresh snow from Friday has also been deposited atop loose snow or surface hoar. The fundament on steep shady slopes at high altitudes is expansively metamorphosed.
Tendency
No significant change in danger levels anticipated
Danger level
Favorable situation
Avalanche danger is low. Triggering a small slab is possible in only few places, most endangered are shady slopes in very steep terrain above 2000m. In isolated cases a small glide-snow avalanche is possible. Isolated small naturally triggered glide-snow avalanches possible.
Snowpack
Atop a melt-freeze crust (or else, bare ground) loosely-packed snow lies deposited. Surface hoar has often been blanketed. On sunny slopes the snow is sticky. The fundament on shady steep slopes is often weak, but the weak layer is varied and the slab shallow.
Tendency
No significant change in danger levels anticipated