Fig. 8From: The 1905 Chamonix earthquakes: active tectonics in the Mont Blanc and Aiguilles Rouges massifsView of the Remuaz scarp along the eastern edge of the Aiguilles Rouges massif. The scarp is outlined by a clear slope break and topographic step across the massif, and locally by ponding (Goliet pond) and by a freshly striated exhumed basal strip (striations) (Alasset 2005)Back to article page