摘要

The excavations carried out in the cave of Santa Ana (Cáceres, Spain), cave of the karstic network of the “Calerizo” of Cáceres, enabled us to know the existence, in stratigraphy, of the three lito-techniques modes which characterize the industrial development of lower and middle Pleistocene in the Iberian Peninsula. On standby of new research, the results obtained until now permit us two work out a diachronic assumption of technical evolution. In the Iberian Peninsula, there are only two karstic systems where we can fallow this technological development; one is the “Sierra de Atapuerca” (Burgos) and the other is the “Calerizo de Cáceres” (Cáceres).