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ike the use of domestic tools or projectiles, flake extraction from blocks of siliceous rock and their subsequent retouching lead to the formation of specific traces, the nature and characteristics of which are largely determined by the technique used. Depending on their nature, these traces can be observed either with the naked eye or with the help of a microscope.

The analysis of knapping wear enriches our knowledge of the skills and technical traditions of prehistoric societies, the evolution of these skills over time, and the appearance and diffusion of innovations related to knapping and the production of stone tools.

Research on prehistoric knapping techniques has been mainly based on experimental collections set up by researchers specialised in knapping of siliceous rocks, and has made it possible to identify combinations of characteristics and traces relevant to the recognition of the techniques employed by prehistoric populations (e.g. Pelegrin 2000; Rots 2010).

At TraceoLab, the study of knapping traces is based on a methodological approach that integrates macroscopic and microscopic observations and builds on experimentation. Experiments are not only designed to create an extensive library of knapping traces corresponding to various prehistoric techniques, but also to better understand the conditions under which these traces form.

In our archaeological research, we have thus far identified hammer residues in an Aterian context, investigated the overlap between production and impact-related damage in the cases of bipolar knapping of quartz in the South African MSA and the manufacture of laterally hafted projectile armatures in the French Final Gravettian, explored the variability in production traces on Early Gravettian tanged points to increase the reliability of hafting wear interpretations, and used production traces as an additional argument to distinguish between individual knappers of Levallois sequences from a Nubian production site in Northeast Africa.

Further reading

updated on 1/20/23

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