Fig. 9From: Three-dimensional modelling of folds, thrusts, and strike-slip faults in the area of Val de Ruz (Jura Mountains, Switzerland)Schmidt net (lower hemisphere) showing 82382 poles to the Earth’s surface as calculated from the digital elevation model, for the entire model area. Best-fit great circle of the orientation distribution is indicated. Filled circle indicates calculated “topographic fold axis” oriented SW-NE, i.e. parallel to the average fold orientation in the areaBack to article page