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Timpone della Motta

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  • 3 chapters

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Through Italy and Iron Age

The hill was abandoned when the Bruttians conquered the region in the fourth century BC.

Geography

The hill is composed of Plio-Pleistocene fan-delta deposits containing thick beds of conglomerated river cobbles, which form its cap rock and several terraces along its slopes. With an elevation of 280 meters above sea level, it overlooks the coastal plain of Sibari and the Gulf of Taranto. It lies on the left (northern) bank of the seasonal Raganello river. Close to the hilltop is the acropolis, which was the location of a sanctuary with three temples. The acropolis was surrounded by a defensive wall. Several of the conglomerate-supported terraces have evidence of settlement and the Macchiabate necropolis lies at the foot of the hill but is separated from it by the Carnevale gully. The ancient Greek city of Sybaris was located at a distance of 15 kilometers to the southeast.

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