In multilayered aquifer systems establishing renewable resources for individual aquifers is a compound problem. The renewable-ness coming mainly from the effective infiltration is taking place directly in the first layer. However the part of these waters indirectly is powering deeper layers as a result of soaking through by semi permeable series dividing aquifers. In the article, on the basis of the regional model of the Gdańsk aquifer system, renewable resources for individual aquifer was analysed. In the Gdańsk region the groundwater appears in Cretaceous, Paleogene-Neogene and Quaternary formations. They create the multiaquifer system.
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