Resumen de Neotectónica en la cuenca del alto Tormes (Sistema Central, Avila): Influencia en la morfología fluvial

C. Pol Méndez, Ana Sánchez del Corral Jiménez, J. Carballeira Cueto

• The High Tormes is caracterized far its aluvial and torrential regimen who ask to a general model of sinuous river complex: straight segments, straight with lateral bars, braided and meandering. The presence of gradient index anomalous high permits to deduce the existence of tectonic activity who fa/Is in the river's patter. The study of relict's boulders bars permits to deduce the structural condicionament of its deposits and the existence of a neotectonics in this section of the Central System after its origen.