https://popups.uliege.be/3041-5535/index.php?id=134 Numéros en texte intégral fr lun., 11 mai 2026 16:06:56 +0200 lun., 11 mai 2026 16:06:56 +0200 https://popups.uliege.be/3041-5535/index.php?id=134 0 https://popups.uliege.be/3041-5535/index.php?id=135 lun., 11 mai 2026 16:07:16 +0200 https://popups.uliege.be/3041-5535/index.php?id=135 https://popups.uliege.be/3041-5535/index.php?id=136 lun., 11 mai 2026 16:07:37 +0200 https://popups.uliege.be/3041-5535/index.php?id=136 https://popups.uliege.be/3041-5535/index.php?id=137 lun., 11 mai 2026 16:07:59 +0200 https://popups.uliege.be/3041-5535/index.php?id=137 https://popups.uliege.be/3041-5535/index.php?id=140 Summarizing and answering the questions from the beginning of this paper one can say that the single Bandkeramik pot-sherd excavated in the Weidental Cave cannot be interpreted as evidence of a permanent early agriculturalist settlement in the hilly region of the Palatinate Forest, but it demonstrates the presence of the early Bandkeramik ("Flomborn") in this region. Perhaps some explorers or "trappers" visited this area, or this sherd could simply represent contact between mesolithic and neolithic groups. Concerning the second inference, one can assume that middlemesolithic (Beuronien C) occupation in the Weidental Cave might probably be much younger than formerly stated. The Weidental Cave inventory might reflect a local late mesolithic tradition without rectangular microliths. If this is true, this time-span between the mesolithic occupation and the Flomborn-expedition would be considerably shortened. In conclusion, we can say that in Rhinehesse-Palatinate in the sixth millennium b.c. not only herders and agriculturalists were living contemporaneously, like the biblical Cain and Abel, but also à third party was still present : the (last) hunter- and gatherer tribes. lun., 11 mai 2026 16:08:15 +0200 https://popups.uliege.be/3041-5535/index.php?id=140 https://popups.uliege.be/3041-5535/index.php?id=142 lun., 11 mai 2026 16:08:29 +0200 https://popups.uliege.be/3041-5535/index.php?id=142 https://popups.uliege.be/3041-5535/index.php?id=144 lun., 11 mai 2026 16:08:43 +0200 https://popups.uliege.be/3041-5535/index.php?id=144 https://popups.uliege.be/3041-5535/index.php?id=145 lun., 11 mai 2026 16:08:58 +0200 https://popups.uliege.be/3041-5535/index.php?id=145 https://popups.uliege.be/3041-5535/index.php?id=148 lun., 11 mai 2026 16:09:19 +0200 https://popups.uliege.be/3041-5535/index.php?id=148 https://popups.uliege.be/3041-5535/index.php?id=150 A blade core of Maastrichtian Hesbaye flint from the Gravettian site of Huccorgne, Southeast Belgium, was refitted to twenty-nine blade fragments, flakes, and pieces of debris. Technological analysis of the lithic operatory chain involved in the reduction of this core, as well as material analysis of internal fissures, suggest that the core was reduced during at least two episodes in spatially discrete portions of the archaeological site. The temporal period between reductions is unknown, but it is posited that the internal crack propagation was the product of exposure to severe cold at the beginning of the Last Glacial Maximum. lun., 11 mai 2026 16:09:43 +0200 https://popups.uliege.be/3041-5535/index.php?id=150 https://popups.uliege.be/3041-5535/index.php?id=153 lun., 11 mai 2026 16:10:05 +0200 https://popups.uliege.be/3041-5535/index.php?id=153