Deformación de terrazas fluviales recientes en la franja costera cantábrica

• Antonio Cendrero Uceda ^[1] ; José Ramón Díaz de Terán Mira ^[1] ; M. Moñino ^[1]
  1. [1] Universidad de Cantabria

     Universidad de Cantabria

     Santander, España

     
• Localización: Geogaceta, ISSN 0213-683X, Nº. 4, 1988, págs. 21-22
• Idioma: español
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• Resumen

  • Evidence of faulting with displacements of several meters in a fluvial terrace 20 m above the present river level has been found in Polaneo, near Santander. The site is located nead a diapir of Triassic clays and salts. This shows that there has been deformation in the area during late Quaternary times, perhaps only in relation to diapir emp/acement.