“…The only red opaque glass sample investigated, 15117RV (Figure 5, Table 2), was featured by a surface golden layer, as well as small spherical holes and craters, indicating the occurrence of a macroscopic alteration quite common in archaeological glass [99]. The core piece displayed as its main elements, found by EDXRF, Si, Pb and Na (with amounts of Furthermore, rutile (TiO 2 , signals at 143, 241, 445 and 610 cm −1 ), and different Si-O bonds of the glassy phase (at 550 and 1093 cm −1 , and also at 480 and 1065 cm −1 ) were identified, together with some calcium and/or aluminum-silicate, incorporating cobalt ions or some alkali sulfate [80,101] as indicated by the signals collected at 459, 616, 637, 996, 1076, 1130 and 1198 cm −1 . Since it is known that cobalt is able to impart a dark blue color in the glass matrix even if present at levels of few µg/g, it can be concluded that the samples' deep blue color is due very likely to its occurrence, as the Co amount was found to range from 0.24 to 0.10 wt.%.…”