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

• C. Pol ^[1] ; A. Sánchez del Corral Jiménez ^[2] ; J. Carballeira Cueto ^[1]
  1. [1] Geociencias. Medio-Ambiente
  2. [2] Departamento de Geología. Facultad de Ciencias. Salamanca.
• Localización: Geogaceta, ISSN 0213-683X, Nº. 6, 1989, págs. 90-93
• Idioma: español
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• Resumen

  • 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.