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An evolutive scheme is proposed for the embayment of Pichilemu. The used methods deal with three theoretical and fundamental principles: the interaction between oblique swell and offset coast, adjustment of sediments to refracted swell and effect of the frandnan transgression. The allostratigraphy of the system was correlated with similar cases visited in the region and withresults on geochronology in some of them. The analyzed system results from an interaction between two principal processes: formation of ria including estuary and production of a zetaform embayment, associated to an estuarine terrace. This form is thought to be formed in the Holocene, starting from its correlation with homologous features of Central Chile. It is found that the two principal morphogenetical processes were sinchronic and that the development of which can be synthesized in four essential moments: effect during the transgression, maximum of the Holocenic transgression filling, effect of balance between recent sea level rise and cortical uplift (formation of the estuarine terrace), and modern effect of shore sediment overload.

Morfogénesis de la ensenada en zeta y de la terraza estuarial asociada en Pichilemu: prototipo para Chile Central