Fig. 10From: The 1905 Chamonix earthquakes: active tectonics in the Mont Blanc and Aiguilles Rouges massifs a Striations observed locally at the base of the Remuaz fault scarp (red rectangle). b Steep striations (pitch of 60°) that are clearly not glacial in origin. c Along a length of 40 m the 20 cm base of the scarp looks rejuvenated and devoid of lichens. d Continuity of striations within a 1.5 m-deep pit at the foot of the Remuaz fault scarpBack to article page