Abstract:In the Avlamış Valley, 10 km north of Eskişehir (NW Anatolia), an undamaged triangular Levallois flake was encountered in a paleosol, 430 cm beneath the ground surface. The artifact has a minimal dorsal retouch on the right margin, and there is a light beige partial patina on the ventral surface. Based on the technological investigations, this artifact was made using the centripetal recurrent Levallois technique. An observation of the trench walls revealed the triple nature of the stratigraphy: an upper gravel… Show more
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