Avalanche danger:
Above 2000:
3 - considerable
Below 2000:

1 - low
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Snowpack structure (2026-03-07):
The snowpack can cool down well overnight and form a melt-freeze crust, which softens again during the day on sunny slopes. In general, the snowpack on sunny slopes is damp or wet up to high altitudes. In shady high altitudes, some of the snow surface is still soft, faceted snow, some of which has already crusted can form. Below this lies a now well-set and connected sequence of compact drift snow layers, but often a crust with angular crystals is still embedded in the upper area. The connection at the transition to the old snow foundation, which consists mainly of deep rime, is still poor to very poor and fractures can still be easily provoked here. Deep and sunny middle layers are often already snowed out.
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