Abstract
ABSTRACT The remarkable excavation of a bone bed deposit at Tourville-la-Rivière has for twenty-five years yielded palaeontological materials, as well as a conjoined core of the Saalian age. Forty flakes were refited onto the core. This important discovery has allowed the precise reconstruction, using technological analysis of volumes, of the whole sequence of de- bitage of a large, elongated flint nodule, to its final abandonment. The quite singular spatial distribution of the conjoined elements has implications for the context of this reduction sequence.
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