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It shows the complexity of the karst area and its local model diversity.
The regimes of the aquifers, landforms and springs were reported in most mountain terrains and the local interactions between the karst aquifer, karst springs, landforms and human action were discussed.
The age of these red deposits are bracketted between Bathonian to Mid-Cretaceous.
Therefore, the spatial relationship of the cleavage with mafic intrusions, in the axial part of the Central High Atlas, suggests that it developed contemporaneously with the emplacement of magmas, probably during Mid-Jurassic times.
Moroccan karst has been the subject of study over the last two decades as a system, where landforms interact with groundwater, springs and human action.
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