The Nerja Cave allows to study the hydrodynamic functioning of the epikarst of the aquifer in which it is developed. The hydrograph of the drip water inside the Cave, versus the precipitations, and the application of the correlatory and spectral analysis to the long series of data precipitation-dripwater flow, shows the inertial behaviour of the epikarst and the importance of the water stored in its hydrodynamic behaviour. The hydrochemical information, particulary the use of K* and ,aO content, confirms these results
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