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The lacustrine system of the rio Grande basin takes place in an area that gathers particularities of both geological and geomorphological points of view at the northwest craton of Sao Francisco River. From the investigation of morphostructural elements, it was intended to present a geomorphology’s view of this system. By using the remote sensing techniques, it was sought to establish the infl uence of both lithology and tectonics in the current dynamics of the drainage and the lacustrine system. The results showed the presence of features like drainage anomalies, basins asymmetry, fl ood plains confi nement, sudden diff erences of drainage density, and the distinction of lakes distribution in terms of form and dimension. The lacustrine system area was compartmentalized into two domains: Domain I with NW-SE morphostructures, and Domain II with the predominance of NE-SW morphostructures and E-W subordinately, concordant to orientations of regional failures, what shows that the activation of ancient failures and the lithological context are important factors for the origin and development of this lacustrine system.

CARACTERIZAÇÃO DA REDE DE DRENAGEM E DO SISTEMA LACUSTRE DA BACIA DO RIO GRANDE: OESTE DA BAHIA - REGIÃO DO MÉDIO SÃO FRANCISCO