Ermias Hagos
Posters: Hydrol Current Res
The groundwater occurrence, flow pattern, rate of recharge and hydrochemical setup in the Tekeze River Basin (TRB) is strongly controlled by the type of rocks and their stratigraphic positions (litho-stratigraphy), geological structures, the topographic setup and the prevailing climatic conditions. The basin constitutes diversified rock types ranging in age from Precambrian to Quaternary and complex tectonic structures. Different sets of folds, faults and lineaments with diverse orientations and associated fractures prominently affect almost all the rock formations in the TRB. Climate and geomorphology of the basin are also diverse.
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