In this research, a hydrogeological model was generated for the analysis of the hydraulic conductivity by means of an indirect geoelectric exploration, through Vertical Electric soundings and direct geotechnical exploration, with the recovery of altered and unaltered down-to-six-meter samples. At the laboratory, samples from the two perforations were characterized and the value of the hydraulic conductivity K (m / d) was determined from a sample from each site by using the Hyprop 2 equipment. The Verifications of the measurement values within the reference ranges were used to generate 2D and 3D models from the thickness and layers from the subsoil. Afterwards, by using the referenced author's proposed methodologies, the hydraulic conductivity (K m / d) was determined through the correlations amongst the values of formation factor (F) and fines content of fines (C).