Fig. 8From: Historical intensity VIII earthquakes along the Rhone valley (Valais, Switzerland): primary and secondary effectsBuilding damage and secondary phenomena in and around the village of Visp after the 1855 event. Comparison of loss on buildings built on rock and soft soil shows no significant differences. Strong secondary phenomena occurred particularly in the northern part of Visp. Modified from Fritsche et al. (2006)Back to article page