Avalanche.report

Thursday 20 February 2025

Published 19 Feb 2025, 17:00:00


Danger level

2200m
Avalanche Problem
Wind slab
2200m
Persistent weak layer
2400m


At high altitudes, caution urged towards small drifts

Avalanche danger is low. Isolated triggerings are possible in extremely steep terrain. In high-altittude pass and ridgeline zones, small-area fresh drifts require attentiveness. They are occasionally prone to triggering but small sized. The danger of being swept along and forced to take a fall outweighs that of being buried in snow masses. The risk of small glide-snow avalances continues to be difficult to assess. Caution urged below glide cracks.

Snowpack

The below-average snowpack is well consolidated by and large. In high altitude pass and rigeline zones, small fresh, often trigger-sensitive snowdrift accumulations require attentiveness, esp. on steep shady slopes these drifts have been deposited. More deeply embedded layers of the snowpack can be triggered in isolated cases above 2400m by large additional loading, esp. in the Silvretta region. On sunny slopes the most recent snowfall is already moist and is forming a melt-freeze crust. During the daytime hours, this crust softens up again.

Tendency

Avalanche danger levels not expected to change significantly


Danger level



Only few danger zones, low danger

Avalanche danger is low. Isolated triggerings are possible in extremely steep terrain. In high-altittude pass and ridgeline zones, small-area fresh drifts require attentiveness. They are often prone to triggering but small sized. The danger of being swept along and forced to take a fall outweighs that of being buried in snow masses. The risk of small glide-snow avalances continues to be difficult to assess. Caution urged below glide cracks.

Snowpack

The below-average snowpack is well consolidated by and large. In high altitude pass and rigeline zones, small fresh, often trigger-sensitive snowdrift accumulations require attentiveness, esp. on steep shady slopes these drifts have been deposited. On sunny slopes the most recent snowfall is already moist and is forming a melt-freeze crust. During the daytime hours, this crust softens up again.

Tendency

Avalanche danger levels expected to remain favorable