Skip to main content
Swiss Journal of Geosciences
Fig. 10 | Swiss Journal of Geosciences

Fig. 10

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

Fig. 10

Schmidt nets (lower hemisphere) showing orientation distribution of Earth’s surface, determined from digital elevation model, for parts of the area. Great circles and filled circles as in Fig. 9. See Fig. 2 for location of the subareas, and Table 1 for comparison of the “topographic fold axes” with structural fold axes from Sommaruga and Burkhard (1997). The difference in trend is small for ENE-trending anticlines (e.g., Mont d’Amin) and partly large for NNE-trending anticlines (e.g., NE part of Chaumont)

Back to article page