Avalanche at the Daunscharte – what the terrain really reveals
The recent avalanche accident on the Stubai Glacier vividly demonstrates how deceptive seemingly "clear" terrain can be. Our 3D visualization makes it clear: it's not the individual point that matters – but the entire catchment area above.
The result:
- Slope angle in avalanche zone: 30 – 40°
- Exposure: Northeast
- Classic scenario for wind-drifted snow and unstable snow layers
Using our color-coded slope gradient display based on our high-resolution terrain model It immediately becomes apparent where avalanche-relevant areas are located. – regardless of where you yourself stand.
Danger from above – even when traveling on flat terrain
The terrain analysis is of course most beneficial to those who travel off-piste: Off-piste skiers, freeriders and ski tourersChoosing your own route allows you to consciously plan for slope gradient, aspect, and runout zones, and better assess risks, always within the context of the current avalanche report. On groomed slopes, the danger can only be influenced to a limited extent – in off-piste terrain, however, good preparation makes a real difference.
But even those venturing onto flat terrain can be endangered by steep slopes above. In the case described, the potential runout zone extends into seemingly harmless areas – precisely where skiers or ski tourers would consider themselves safe.
Our 3D map helps answer exactly these questions:
Where are the potential crack initiation points?
In which direction would an avalanche travel?
Which zones are potentially within the run-off corridor?
This makes it possible to recognize whether you are in a danger zone – even without having to enter a steep slope yourself.
With our app You always have this information with you when freeriding and ski touring.
