Raman spectroscopy has been used to study the molecular structure of a series of selected uranyl silicate minerals including weeksite K 2[(UO 2) 2(Si 5O 13)]·H 2O, soddyite [(UO 2) 2SiO 4·2H 2O] and haiweeite Ca[(UO 2) 2(Si 5O 12(OH) 2](H 2O) 3 with UO 2 2+/SiO 2 molar ratio 2:1 or 2:5. Raman spectra clearly show well resolved bands in the 750–800 cm −1 region and in the 950–1000 cm −1 region assigned to the ν 1 modes of the (UO 2) 2+ units and to the (SiO 4) 4− tetrahedra. Soddyite is characterized by Raman bands at 828.0, 808.6 and 801.8 cm −1, 909.6 and 898.0 cm −1, and 268.2, 257.8 and 246.9 cm −1, attributed to the ν 1, ν 3, and ν 2 (δ) (UO 2) 2+, respectively. Coincidences of the ν 1 (UO 2) 2+ and the ν 1 (SiO 4) 4− is expected. Bands at 1082.2, 1071.2, 1036.3, 995.1 and 966.3 cm −1 are attributed to the ν 3 (SiO 4) 4−. Sets of Raman bands in the 200–300 cm −1 region are assigned to ν 2 (δ) (UO 2) 2+ and UO ligand vibrations. Multiple bands indicate the non-equivalence of the UO bonds and the lifting of the degeneracy of ν 2 (δ) (UO 2) 2+ vibrations. The (SiO 4) 4− tetrahedral are characterized by bands in the 470–550 cm −1 and in the 390–420 cm −1 region. These bands are attributed to the ν 4 and ν 2 (SiO 4) 4− bending modes. The minerals show characteristic OH stretching bands in the 2900–3500 and 3600–3700 cm −1.