Picture of a large Levallois flake (on the left) and a Levallois core (right). (IMAGE)
Caption
The flake was struck from the core in a much earlier stage of the “biography” of the core, when it was significantly larger. Other flakes produced between the large flake and the final core were also recovered at this site, one of the minimally 250,000 years old flint and bone scatters excavated in the 1980s by Leiden archaeologists at Maastricht-Belvédère (The Netherlands).
Credit
Leiden University
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