Abstract
Thanks to recent research and the re-evaluation of the archaeological material coming from older research, the Mousterian of Greece has started to become better known. Aside the surface findings, which testify the presence of Mousterian throughout the entire continental Greece, only five Middle Paleolithic sites have been excavated. Almost every remnant has been dated to the last ice age. All lithics belong to the “typical” Mousterian, while the Quina Mousterian has not been certainly testified. The Levallois method is almost always present, more or less frequent, but always dominated by non-Levallois methods. The recurrent variations, mostly centripetal, have been more frequently used. The “Micromousterian” of Asprochaliko is the only lithic assemblage from which the Levallois method is absent.
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