“…In fact, and in spite of their great potential interest, provenance studies on igneous and metamorphic rock raw materials for Iberian archaeological objects have been only occasionally conducted because of (i) the rarity of research projects focused on the survey of the primary geological outcrops for those kinds of raw materials and evidence of their archaeological use; (ii) general prejudices about the use of natural preforms of igneous and/or metamorphic rocks collected from pebble‐rich river and/or beach sedimentary deposits; and (iii) lack of knowledge about identifying the technical marks produced by knapping on igneous or metamorphic rocks (Orozco‐Köhler, ; Risch, ; Risch, and Martínez, ). However, occasional significant studies from sites in the southern half of the peninsula have offered lithological characterization of archaeological utensils by means of petrographic and/or geochemical analyses that have allowed the identification of provenance, such as amphibolite complexes located in the Ossa Morena zone, western Iberia (Lillios, , ; Red, Grapes, & Lillios, ), amphibolite, and/or gabbro from the Internal Zones of the Betic Cordillera of southern Spain (Domínguez‐Bella, Pérez, & Morata, ; Domínguez‐Bella, Pérez, Ramos, Morata, & Castañeda, ; Orozco‐Köhler, ; Pérez Rodríguez, Domínguez‐Bella, Morata, & Ramos, ; Ramos Muñoz et al., ) and eclogite from the Nevado‐Filábride Domain of the Internal Zone of the Betic Cordillera (Carrión et al., ; Carrión, & Gómez‐Pugnaire, ).…”