“…The Cretaceous int from Monte Tabuto ( g. 1a, 1c) displays a light sandy colour with a coarse surface, while that from Monterosso Almo was a Miocene ne-grained int ( g. 1d-e) (Nicoletti, 1990(Nicoletti, , 1997. The selection of int from such speci c areas was due to the initial constitution of an experimental collection suitable for analysing contexts in southeastern Sicily (Magro et al, 2021;Militello et al, 2018;Sferrazza, 2018Sferrazza, , 2022Sferrazza, , 2023Sferrazza-Militello, 2024). Instead, the test dataset (supplementary materials A) had Sicilian and non-Sicilian archaeological artefacts.…”