Abstract
Several geoscientists in the past have mentioned the presence of pebbles, that have originated from the metamorphosed formations of the lower tectonic units of Péloponnèse (Ama and Mani units), in the outcrops of the post-alpine deposits of Pylia penninsula. As the present physicogeographical appearance of SW Péloponnèse does not justify the existence of those pebbles in the post-alpine deposits of Pylia, since Arna and Mani units outcrop only at the Mani penninsula, an efford is made for the interpretation of the paleogeographic evolution of the greater area and the conditions of deposition of those formations.
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