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Abstract
With the investigation of determinates parameters in the mineral waters of the province of Valencia, we are looking for the possible relation between the composition of those waters and the geological characteristics of the zone. From the result of the analysis we deduce that the water s with minus mineralization are found al the oldest Buntsandstein terrenes of the north zone of the province, while the waters with more mineralization are found at Keuper terrene. The most mineral water s and potable waters are found at Triassic terrene or Cretaceous terrenes. About the waters to drink that are work commercially predominate the bicarbonated-caIciumed and bacteriologicaly they used to be correct in the work is correct. From the Miocene and Quaternary emanate water s with increased sulphate.
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