Avalanche.report

Sunday 23 February 2025

Published 22 Feb 2025, 17:00:00


Danger level



Favorable conditions

Isolated avalanche triggerings by winter sports enthusiasts possible in extremely steep terrain. In high-altitude pass and ridgeline terrain, small snowdrifts require attentiveness, they are often still prone to triggering. The danger of being swept along and forced to take a fall outweighs that of being buried in snow masses. Danger of small (where snowfall has been heavy also medium-sized) glide-snow avalanches on steep grass-covered slopes or rocky plates remains difficult to asses. Caution urged below glide cracks.

Snowpack

The below-average snowpack is well consolidated b and large. In high altitude pass and ridgeline zones, small fresh, often trigger-sensitive snowdrift accumulations require attentiveness. Esp. on steep shady slopes these drifts have been deposited atop loose snow and are prone to triggering. High-altitude shady slopes are often still powdery, elsewhere the snowpack is often with breakable crusts, sometimes wind crusts are capable of bearing loads. On sunny slopes, a melt-freeze crust. During the daytime hours, this crust softens up again.

Tendency

Avalanche danger levels not expected to change significantly


Danger level

2200m
Avalanche Problem
No distinct avalanche problem
2200m
Gliding snow
2200m


Increasingly frequent glide-snow avalanches, otherwise favorable conditions

Danger of small (where snowfall has been heavy also medium-sized) glide-snow avalanches on steep grass-covered slopes or rocky plates remains difficult to asses. Caution urged below glide cracks. Otherwise avalanche dange ris low. Isolated triggerings by winter sports enthusiasts in extremely steep terrain are possible. The danger of being swept along and forced to take a fall outweighs that of being buried in snow masses.

Snowpack

The below-average snowpack is well consolidated by and large. In high altitude pass and ridgeline zones, small fresh, often trigger-sensitive snowdrift accumulations require attentiveness. Esp. on steep shady slopes these drifts have been deposited atop loose snow and are prone to triggering. High-altitude shady slopes are often still powdery, elsewhere the snowpack is often with breakable crusts, sometimes wind crusts are capable of bearing loads. On sunny slopes, a melt-freeze crust. During the daytime hours, this crust softens up again. In recent days increasingly frequent fresh glide cracks and glide-snow avalanches have been reported.

Tendency

Avalanche danger levels not expected to change significantly