Quaternary fluvial network of the piedmont of Western Sierra Morena
DOI:
https://doi.org/10.18172/cig.993Abstract
The main alluvial terraces of the southwestem atlantic area are defined and also the evolution ojtheirs rivers. The geomorphological evidences shows a NE-SW fluvial directions in the begining and N-S tracing later, controlled by tectonic deforrnations and the Quatemary sea level fluctuations.Downloads
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