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The article investigates the processes of water percolation in the Mediterranean karst area. It notes that the drip response of stalactites in a karstic cave in Mount Carmel, Israel was measured. It also mentions that the study of recharge processes involved hydrometric measurement, and tracers such as electrical conductivity and bromide. The results showed that filling of the unsaturated zone is an important precondition for the onset of significant water percolation and recharge.