Figure 9. Evolution of the piezometric level on both sides of the faults: Sébikotane fault between the Sébikotane and Nothern Pout compartments (a) and between Sébikotane and Diass compartments (b) Pout fault between the Maastrichtian of Diass and the Palaeocene of Southern Pout (c), the Maastrichtian of Diass and that of Southern Pout (d), the Maastrichtian of Diass and the Paleocene of Mbour and the Maastrichtian of Diass and that of Mbour (e); Thies fault in the North (f) and South of the system (g)

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Hydrogeological Characterization and Hydrodynamic Behaviour of the Overexploited Diass Aquifer System (Senegal) Inferred from Long Term Groundwater Level Monitoring

Diakher Hélène MADIOUNE, Moctar DIAW, Ibrahima MALL, Philippe ORBAN, Serigne FAYE, Alain DASSARGUES

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