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Karst aquifers in semi-arid regions are vital yet exceptionally vulnerable lifelines. This study investigates how
tectonic, geomorphological, and climatic factors control the dynamics of karst springs in the El Menzel Causse
(Middle Atlas, Morocco). Using an integrated approach that combines field investigations, remote sensing, and
quantitative hydro-climatic analysis, we identify the mechanisms driving the system’s severe decline. Results
indicated that the structural architecture of the major fault systems in the North Middle Atlas Fault (NMAF) and
the Median Middle Atlas Fault (MMAF), governs the spatial distribution of more than 50 springs, which occur
preferentially within highly permeable fault damage zones. However, the aquifer is
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