Fig. 7

View from Zeneggen (see Fig. 1) looking eastwards along the deep trench called Staldbachgraben. Red dashed line shows part of the assumed surface trace of the Hotée fault (Joris, personal communication), which could have ruptured during the 1855 Visp earthquake (Fig. 1). Red arrows show where geomorphological indications for a separation between hanging-wall, on which Unterstalden is located, and footwall, on which Oberstalden is located, have been observed. This figure was taken from http://www.heidadorf.ch