El poblamiento tardoneolítico y calcolítico en el estuario del Tinto-Odielel yacimiento La Orden-Seminario (Huelva)

Laburpena

The prehistorics structures documented in the site “La Orden-Seminario” of Huelva are set chronologically in the transition Neolithic- Chalcolithic (final IV Millennium- early III millennium BP). This phase is the first of occupation that’s stated inside the site La Orden-Seminario of Huelva and it’s outlined as one of the most important of the zone, as much for its area as for the condition of preservation that present the deposits and located structures. The settlement final Neolithic-Chalcolithic of the estuary Tinto-Odiel from Huelva has making up since the ‘80s one of the most mentioned clichés of the Iberian historiography related to the recent prehistory because of the excavation from Papa Uvas (Aljaraque). The special area of the archaeological work in “La Orden-Seminario” offers an excellent counterpoint and expectative of studies micro and semi-micro spatial unique due to the conditions of conservation.