Quaternary fluvial network of the piedmont of Western Sierra Morena
oleh: J. Rodríguez Vidal, L. Cáceres Puro, A. Rodríguez Ramírez
| Format: | Article |
|---|---|
| Diterbitkan: | Universidad de La Rioja 2013-05-01 |
Deskripsi
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.