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J. P. Siwek
Fig. 13.3 Water conductivity of springs in the Ryjak stream catchment (Beskid Niski Mountains)
according to geology (from Lasek [24], changed). 1—oligocen thick-layered sandstones and shales
(magura layers), 2—eocenic shales with sanstone insert (magura layers), 3—eocenic thick-layered
sandstones (magura layers), 4—eocenic shales and thin-layered sandstones (hieroglific and magura
layers), 5—eocenic shales and thin-layered sandstones (hieroglific and beloweskie layers), 6—
eocenic varicolored shales, 7—eocenic shales with sandstones-insert and shales with thin-layered
sandstones (magura and hieroglific layers), 8—watershed, 9—streams