Abstract

Anglona is the site of a prehistoric, Hellenistic and medieval settlement overlooking the Ionian Sea, 60 km. south-west of Taranto (Fig. 1). In 1965 we carried out a short trial excavation at Anglona on behalf of the Soprintendenza alle Antichità for Lucania. The excavation was of an exploratory nature. The site has since been excavated on a larger scale by the German Archaeological Institute, but the results obtained by ourselves were sufficient to call for a brief report. Anglona is a hilltop site which today supports only one standing monument, a twelfth-century church.However, it has long been known that a medieval settlement existed here and it is thought that the site was also that of Hellenistic Pandosia. Before excavation began, surface finds suggested that the site was also occupied in the prehistoric period. The suspicion was confirmed by the discovery of abundant Late Bronze or Early Iron Age material in securely stratified deposits.Anglona is situated on a long narrow ridge which runs down to the coast, 12 km. to the east. The topography of the region falls into three distinct zones, each roughly parallel to the coast. Nearest the sea is a low coastal strip, up to 7 km. wide, composed of fossil dunes and alluvium. Behind the strip lies a zone of eroded sand and gravel hills. The loosely cemented deposits weather rapidly, creating low cliffs and steep-sided ravines. Finally, behind the hills, is the mountainous hinterland of Basilicata. Within the space of only 30 km., between Metaponto and Siri, no fewer than five rivers enter the Ionian Sea. The rivers drain a large area of Basilicata and, although sluggish today, at times of increased rainfall they carried a considerable volume of water. The rivers have cut broad valleys through the gravel hills, leaving a series of irregular ridges running at right angles to the coast.

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