Research has shown that the distribution of springs in flysch areas is affected by complex determinants consisting of interdependent geological and morphological factors. The most important factor appears to be the layering of rocks relative to the slope of the given mountain, which affects both the number and discharge of springs. Some springs arise due to tectonic faults and fractures. In addition, the very presence of any slope positively affects the probability of the occurrence of a spring in a given area.

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