TL and WFL Sites
The loess, loess-derived sediments and the many intercalating fossil soils overlying the "Rocourt soil complex" and the "Warneton soil complex" belong to the Weichselian s.s. and represent the terrestrial equivalent of MIS 4, 3 and 2. The TL-R-Site, the TL-GF-Site and the WFL-Site can all be dated to the Middle Weichselian (MIS 3) and they all reveal the presence of lithic material in connection with the remains of large mammals. The lithic assemblage of those sites is clearly characterised by the presence of large Levallois products in association with Quina sidescrapers.
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