Fig. 7
From: The 1905 Chamonix earthquakes: active tectonics in the Mont Blanc and Aiguilles Rouges massifs
Aerial view of the narrow N60° trending fault break in the steep northeastern flank of Gros Nol (2458 m) located at the southwestern end of the Vallorcine-Valais fault zone (tip of the aftershock area of Vallorcine 2005 Mw = 4.7 earthquake, Frechet et al. 2011). Bedrock break predates the Vallorcine 2005 main shock as evidenced in October 2005 and 1973 photos taken from the point shown by the red star