Resumen de Deformación de terrazas fluviales recientes en la franja costera cantábrica
Antonio Cendrero Uceda, José Ramón Díaz de Terán Mira, Manuel Moñino Sáez
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.
