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Fig. 9 | Swiss Journal of Geosciences

Fig. 9

From: Three-dimensional modelling of folds, thrusts, and strike-slip faults in the area of Val de Ruz (Jura Mountains, Switzerland)

Fig. 9

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 area

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