Avalanche danger • Lechtaler Alpen Mitte region • 2025/26
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Lechtal Alps Central
Lechtaler Alpen Mitte
Wed 1 Apr
Day Risk Profile
2
Moderate
below treeline
3
Considerable
above treeline
Avalanche Problems
Above 2200 m
Considerable
(3)
Dry avalanches
· all day
Persistent weak layersSlab3
N, NE, E, W, NW
above 2200m
LargeFewPoor
GM.6GM.1
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.
Easy to spot - the snow is fresh. Look at recent avalanche activity in similar terrain, and pay attention to how much new snow has fallen in the last three days. Critical loading depends on temperature, wind, and what was on the surface before the storm. SLF advises waiting until the Snow deposited on the ground in a multiplicity of layers.EAWS glossary has had time to bond before committing to steep terrain in fresh snow.
Easy to spot - the snow is fresh. Look at recent avalanche activity in similar terrain, and pay attention to how much new snow has fallen in the last three days. Critical loading depends on temperature, wind, and what was on the surface before the storm. SLF advises waiting until the Snow deposited on the ground in a multiplicity of layers.EAWS glossary has had time to bond before committing to steep terrain in fresh snow.
New snow and wind slabs represent the main danger.
The large quantity of fresh snow and the extensive wind slabs can be released easily, even by a single winter sport participant,. The fresh and older wind slabs are covered with new snow and therefore difficult to recognise. Avalanches can reach medium size, especially above the tree line. 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 serve as an alarm indicating the danger. Avalanches can in isolated cases penetrate near-ground layers of the snowpack and reach large size, especially on very steep west, north and east facing slopes above approximately 2200 m. In addition small to medium-sized loose snow avalanches are possible, in the event of prolonged bright spells especially on extremely steep slopes. Isolated small and medium-sized gliding avalanches are possible in particular on very steep grassy slopes.
Outlook
→Constant avalanche danger
2 April 2026
The avalanche danger will persist.
Snowpack & Weather
Snowpack▾
Over a wide area 30 to 50 cm of snow, and even more in some localities, has fallen. The strong wind has transported the new snow significantly. In some cases the various wind slabs have bonded still only poorly together. The Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary will be weakly bonded in some places, especially on west, north and east facing slopes above approximately 2200 m.
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