“…Large flakes are commonly used in some sites, whereas in North Africa at Thomas Quarry I level L (1 Ma), Sidi Abderrhamane STIC L1 L2/level F extension site or Tighenif (800 ka), LCTs are partial, picklike and frequently unifacial on pebbles and flakes (Raynal et al, 2001(Raynal et al, , 2011. Some of these features are common to la Noira; for instance, twisted bifaces on obsidian are observed at Gombore II (800 ka), mainly on large flakes (Gallotti et al, 2010). Modes of shaping of some pieces at la Noira are also similar to standardized LCTs on flakes from Isenya (700 ka) (Roche et al, 1987(Roche et al, , 1988Texier and Roche, 1995;Texier, 2001).…”