Glacier Flims Laax Falera
Fussballplatz der Alpen - dem Gletscher sei Dank
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Adventure Flims - Alpine formation simply explained - POI 5
The glacier was able to remove the soft flysch rocks in the area of the upper Segnesboden more easily than the limestones south of today's plain.
A natural terrain hollow was created, which filled with rock debris after the melting of the Segnes Glacier.
The glacier stream distributed this rock debris evenly over the entire plain. At the end of the plain, the stream tied a path through the limestones, creating a deep gorge.
Responsible for this content UNESCO-Welterbe Tektonikarena Sardona.
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