ABSTRACT
However, the ‘signal’ is likely to be weak: it is doubtful, for example, how much of Kanzi’s stone flaking (Toth et al. 1993) would be recognized as such if found in Pliocene contexts in the Rift Valley.
However, the ‘signal’ is likely to be weak: it is doubtful, for example, how much of Kanzi’s stone flaking (Toth et al. 1993) would be recognized as such if found in Pliocene contexts in the Rift Valley.