Forest represents an ecosystem, giving many benefits to man. In addition to its production function the forest plays an increasingly important role in the production of resources, accumulation, and finally, the groundwater reserves.A rare combination of geological, topographic, climatological and pedological factors has contributed to the creation of the important water management area in the territory of the Teplá dolina valley, Veľká Fatra Mountains, resulting in the presence of wells with high quality of groundwater resources. The aim of the presented work was to know the patterns, as well as the factors that contributed to their creation.We found out, that the formation of waterborne structures in this area was conditioned by existence of the siliciclastic material in the slope deposits, covering the carbonates of Mesozoic age of the veporikum unit, probably representing the insoluble carbonate residues (at the silt and clay fraction), that was cemented with organic matter, due to presence of Ca2 + and Mg2 + cations, into the abundand soil aggregates. Water movement, based on electrical resistivity tomography measurements, was carried out at shallow levels, usually at level Bv horizons of modal cambisoils, which, on the basis of soil particle analysis, fall into the field of silty-loam soils.