Abstract
Heat treatment of silicate toolstone was performed prehistorically, which we assume was to improve characteristics desired in flintknapping, such as increased brittleness and more predictable and controlled conchoidal fracture. However, despite research into heat treatment spanning 50 years, the mechanisms by which stone was improved, and the reasons why people did it, remain unclear. In this study, experiments were designed to test two potential outcomes of heat treatment for Pennsylvania jasper. First, does heating reduce the disruptive effect of macroscopic impurities and flaws on controlled flaking? Second, does heating increase the stone’s brittleness as suggested by Crabtree and Butler in 1964? Such physical alterations would improve the quality of lithic material but may not always occur in high quality stone. The results of these experiments are used to hypothesize the expected heat treatment outcomes sought after by prehistoric flintknappers.
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