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.
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