The Calatayud Tertiary basin, shows a concentric facies distribution that represent the transition from the detritical marginal facies to evaporitics-carbonated in the middle of the basin. The marginal detritics sediments constitute the acuifer in the ME of this zone. An example of this king of acuifer is the one from Marivella, placed near Calatayud. We analize herein the special situation of this acuifer, its hidrogeological behaviour and the disturbs¿? that the antropic action is causing on it. The constant extraction by the inhabitants of this zone, the farming production and the new construction of a railway tunnel has implied an important falling off in the acuifer reservoir. In this vork some measures for helping the recuperation of this acuifer are propose.
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