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Glarus Thrust at Martin's Hole
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Description
Two weak layers intersect in the legendary Martin's Hole: a soft, flat, dark marl layer and a steep fracture surface. Erosion in this area was able to quickly remove the limestone, creating Martin's Hole with a diameter of more than 15 metres. On two days each in spring (13-14 March) and autumn (1-2 October), the sun's rays hit the church of Elm through Martin's Hole.
Directions
Public Transport
By train to Chur, then by post bus to Flims Bergbahnen, by FlemXpress to the Segneshütte, from there on foot (see directions)
Directions
From Zurich on the A3 exit 18 Reichenau, continue on the E19 to the Flims exit, parking garage at Flims Bergbahnen, from there with the FlemXpress to the Segneshütte.
Contact
Glarus Thrust at Martin's Hole
Responsible for this content: UNESCO-Welterbe Tektonikarena Sardona.
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