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Texel Mountains

Alta Val Passiria

Wed 18 Feb

Updated off-schedule

The provider reissued this bulletin at 18 Feb 09:27 UTC, outside the normal publication cycle.

Day Risk Profile

Moderate
below 2100m
High
above 2100m

Avalanche Problems

Above 2100 m

High (4) Dry avalanches · all day
Dry snow level 4 Persistent weak layers Slab 4
N, NE, E, W, NW
above 2100m
Large Many Very poor
GM.1 GM.6
Field notes

Persistent Snowpack layer in which the crystals are poorly bonded and the layer has the potential to fail. Typical crystals in dry weak layers causing avalanches are : precipitation particles; surface hoar; faceted crystals; hollow crystals; graupel. Generally >1mm in size, loose grains with few bonds Wet weak layers can be formed by all snow crystal/grain types.EAWS glossary are very challenging to recognise. Distinctive noise (resembling a “whumpf” sound) occurring when a weak layer beneath a slab collapses. The air of the weak layer is forced outside the snowpack, with the resulting whumpf sound being heard. The sound usually indicates an unstable situation and can be accompanied by surface cracking. A whumpf is a clear avalanche alert.EAWS glossary sounds and shooting cracks are typical when present, but you can have a serious weak layer with no warning signs at the surface. Knowledge of how the Snow deposited on the ground in a multiplicity of layers.EAWS glossary has evolved is essential. SLF's travel advice is direct: travel conservatively, avoid terrain where the consequences of being caught are large, and treat the history of weather and snow as more important than what you can see today. Read the full bulletin.

Source: SLF Avalanche Bulletin Interpretation Guide

Above treeline

High (4) Dry avalanches · all day
Dry snow level 4 Wind slab Slab 4
All aspects
above treeline
Medium Some Poor
GM.1 GM.6
Field notes

Look for fresh snow deposits on Slope facing downwind/ wind sheltered aspect. Snow deposits can attain several times average snow depth.EAWS glossary, in Usually a steep, elongated, eroded trench; typically prone to snowdrift accumulation.EAWS glossary and Rounded or elongated concavity; typically tending to accumulate snowdrift.EAWS glossary, and behind ridgelines and abrupt changes in terrain — these are where the wind has loaded the snow into slabs that are easy to trigger. Recent avalanches, shooting cracks under your weight, and Distinctive noise (resembling a “whumpf” sound) occurring when a weak layer beneath a slab collapses. The air of the weak layer is forced outside the snowpack, with the resulting whumpf sound being heard. The sound usually indicates an unstable situation and can be accompanied by surface cracking. A whumpf is a clear avalanche alert.EAWS glossary sounds are clear confirmations of the problem. The safest move is to avoid wind-loaded terrain entirely. NB wind signs alone don't always mean an avalanche problem exists, and the age of drifted snow is hard to judge.

Source: SLF Avalanche Bulletin Interpretation Guide

Avalanche Activity

Weak layers in the old snowpack can be released very easily. Fresh wind slabs are to be evaluated critically.

Distinct Snowpack layer in which the crystals are poorly bonded and the layer has the potential to fail. Typical crystals in dry weak layers causing avalanches are : precipitation particles; surface hoar; faceted crystals; hollow crystals; graupel. Generally >1mm in size, loose grains with few bonds Wet weak layers can be formed by all snow crystal/grain types.EAWS glossary in the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary can be released easily by individual winter sport participants. This applies on west, north and east facing slopes above the tree line. Avalanches can reach large size in isolated cases. Caution is to be exercised in particular on north and east facing slopes above approximately 2200 m. Here such Locations delineated by aspect or altitude where avalanches can trigger and people or objects are at risk.EAWS glossary are more widespread. Distinctive noise (resembling a “whumpf” sound) occurring when a weak layer beneath a slab collapses. The air of the weak layer is forced outside the snowpack, with the resulting whumpf sound being heard. The sound usually indicates an unstable situation and can be accompanied by surface cracking. A whumpf is a clear avalanche alert.EAWS glossary sounds and the formation of shooting cracks when stepping on the Snow deposited on the ground in a multiplicity of layers.EAWS glossary and fresh avalanches serve as an alarm indicating the danger. Remotely triggered avalanches are possible. In addition the fresh wind slabs of the last few days in Usually a steep, elongated, eroded trench; typically prone to snowdrift accumulation.EAWS glossary and Rounded or elongated concavity; typically tending to accumulate snowdrift.EAWS glossary, and behind abrupt changes in the terrain are prone to triggering in some locations. Such avalanche prone locations are to be found on north, east and southeast facing slopes above the tree line. Individual avalanche prone locations are to be found in areas close to the tree line. The prevalence of avalanche prone locations and likelihood of triggering will increase with altitude. The avalanche situation is a little more favourable in highly frequented terrain.

Outlook

Constant avalanche danger

19 February 2026

Weak layers in the old snowpack represent the main danger. <br/> <br/> Thursday: <br/> Up to 10 cm of snow, and even more in some localities, will fall. The wind will be strong to storm force at times. The new snow and wind slabs are bonding poorly with the old snowpack in many places in all aspects.

Snowpack & Weather

Snowpack
Over a wide area 20 to 40 cm of snow, and even more in some localities, has fallen since Sunday. The wind was strong to storm force at times. The Snow deposited on the ground in a multiplicity of layers.EAWS glossary will be prone to triggering. The new snow and wind slabs are bonding only slowly with the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary. In some places various wind slab layers are lying on Transparent, frequently flat crystals forming on the snowpack when moist air settles on the surface. It forms most often during cold, clear, humid nights. Once it is blanketed by fresh fallen snow, surface hoar is one of the most critical weak layer. See also: www.snowcrystals.itEAWS glossary. Distinct Snowpack layer in which the crystals are poorly bonded and the layer has the potential to fail. Typical crystals in dry weak layers causing avalanches are : precipitation particles; surface hoar; faceted crystals; hollow crystals; graupel. Generally >1mm in size, loose grains with few bonds Wet weak layers can be formed by all snow crystal/grain types.EAWS glossary exist in the bottom section of the snowpack on west, north and east facing slopes.

Source

ALBINA

Issued

18 Feb 09:27 UTC

Valid until

18 Feb 16:00 UTC

Next update

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Schedule

Off-schedule

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