STREFOWOŚĆ ZAWODNIENIA W PROFILU PIONOWYM FLISZU PODHALAŃSKIEGO W ŚWIETLE BADAŃ WODOCHŁONNOŚCI (z 3 fig.)

Abstract

THE ZONES OF WATER PERMEABILITY WITH DEPTH IN THE FLYSCH DE POSITS OF PODHALE IN THE LIGHT OF EXAMINATION OF WATER-STORAGE CAPACITY (with 3 Figs.)

Abstract. The paper presents the analysis of the variability of water permeability with depth in the flysch deposits in the region of the Podhale Basin (Inner Carpathians). In the light of the perfomed studies it has been stated that the fractured and permeable 80–100 m thick zone is very important for the water flow in the rocks of the Podhale flysch. The thickness of this zone is diversified and depends mainly on lithologic development of the flysch deposits and on their morphological position. In the shale Szaflary and Zakopane Beds (also beds from Brzegi) its thickness reaches only 30–50 m while in the sandstone Chochołów Beds — 80–100 m. The obtained results are comparable with the regional statistic evaluation of such data from the region of the Outer Carpathians.