The chalcolithic cemetery at Manerba del Garda

Author:

Barfield L. H.

Abstract

The south-western shoreline of Lake Garda is for the most part low and shelving, but at Manerba an outcrop of triassic limestone forms a dramatic, high promontory projecting into the lake (FIG. 1 ). This geological formation is stepped in two levels : the higher, inland part, called the ‘Rocca’, occupied during the Neolithic, Bronze Age, Iron Age and Roman periods, as well as being the site of a medieval castle (Borrello, 1973 ; Brogiolo, 1973), and the lower level, the Sasso, comprising a sheer cliff dropping some 90 m down to the lake edge, with, at its foot, a chalcolithic cemetery, as well as traces of both earlier and later use by man.

Publisher

Cambridge University Press (CUP)

Subject

General Arts and Humanities,Archaeology

Reference23 articles.

1. Riparo Val Tenesi, Manerba, Scavi;Barfield;Benacus,1978

2. La Grotta del Leone;Radi;Antichità Pisane,1974

3. La Grotta sepolcrale di S. U-uiseppe di Rio Marina nell lIsola d?Elba?notizia preliminare;Cremonesi;Atti dells Societa Toscana di Scienze Naturali,1967

4. L’eneolitico e l?antica eta del bronzo in Lombardia;Atti del I Convegno archeologico regionale della Lombardia,1980

5. Patterns of North Italian trade 5000–2000 BC in (eds) G. Barker and R. Hodges;Archaeology and Italian Society; Papers in Italian Archaeology,1981

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