“…Micro‐Raman spectroscopy carried out on the dark blue glass revealed the presence of different silicate bands in most samples: 170, 229, 329, 415, and 467 cm −1 in sample 7; 374, 1,062, and 1,129 cm −1 in sample 11; 274, 383, and 397 cm −1 in sample 12; and 195–196, 245, 309, 327, and 354 cm −1 in sample 14 (Figure c). As previously mentioned, these silicate bands are most likely the result of the rearrangement of the silicate network following selective leaching .…”