Avalanche danger above the timberline is MODERATE. Slabs, mostly small-sized, can trigger particularly on very steep and extremely steep north, east and south-facing slopes by minimum additional loading. Isolated small glide-snow and loose-snow avalanches can trigger naturally.
Snowpack
On top of a shallow and relatively compact snow cover, less than 30cm of snow and drifts (with embedded graupel) lie deposited. The border to the old snowpack can serve as a weak layer, more deeply embedded layers are unlikely to trigger.
Tendency
Avalanche danger levels to gradually recede
Danger level
treeline
Avalanche Problem
Wind slab
Treeline
Circumvent snowdrift accumulations
Avalanche danger above the timberline is MODERATE. Slabs, mostly small-sized, can be triggered even by minimum additiional loading both near to and distant from ridgelines and behind protruberances in the landscape on north, east and south facing slopes. If they fracture down to more deeply embedded layers in the snowpack the releases can grow to medium size. Isolated sm glide-snow and loose-snow avalanches can trigger naturally.
Snowpack
On top of a shallow and relatively compact snow cover, less than 30cm of snow and drifts (with embedded graupel) lie deposited. The border to the old snowpack can serve as a weak layer, more deeply embedded weak layers are triggerable only in isolated cases above 2200m.
Avalanche danger above 2000m is MODERATE. Small-to-medium slab avalanches can be triggerd by minimum additional loading in places on north and east facing slopes, higher up also on south-facing slopes. The snowdrift accumulations are generally easy to recognize. Size and frequency of danger zones tend to increase with ascending altitude. As of 2300m, releases can fracture down to more deeply embedded layers inside the snowpack and grow to larger size. Small glide-snow and loose-snow avalanches can trigger naturally.
Snowpack
The snow cover has below average depths, is highly irregular and the layering is rather poor. With ascending altitude, increasingly frequent crusts with immediately adjacent faceted crystals are evident, mostly triggerable by large additional loading. On the surface there is less than 40cm of snowdrift, poorly bonded with the old snowpack.
