The assignments of Raman bands in the spectra of silicate and germanate glasses, including SiO2, GeO2, Rb2Si4O9, NaFe3+Si3O8, anhydrous and hydrous albite (NaAlSi3O8) and anhydrous and deuterated Ge‐albite (NaAlGe3O8) and Ge‐jadeite (NaAlGe2O6), were re‐examined in the light of new information from Raman measurements at high pressures and temperatures. On the basis of polarized Raman spectra of single‐component (e.g. SiO2 and GeO2) glasses, it is demonstrated that the νas(T–O–T) mode (where T represents tetrahedrally coordinated cations, Si or Ge) gives rise to LO–TO splitting. The depolarized nature of the νas(T–O–T) LO–TO doublet in the Raman spectra of SiO2 and GeO2 glasses reflects the fact that the local site symmetry of T cations is close to Td. Persistence of the νas(T–O–T) LO–TO doublet slightly above the melting temperature demonstrates that significant intermediate range order exists even in the high‐temperature liquids. Likewise, in the spectra of NaFe3+Si3O8 and NaFe3+Si2O6 glasses, the high‐wavenumber νas(T–O–T) bands exhibit a depolarized character characteristic of a three‐dimensional network. The depolarized nature of the νas(T–O–T) bands indicates that the local site symmetry of the T cation is close to Td and that the triply degenerate (F) character of the νas(T–O–T) is preserved. Additionally, a significant shift in the position of the νas(T–O–T) mode on substituting NaFe3+ for Si4‐ reflects strong vibrational coupling of FeO4 and SiO4 tetrahedra in the glass. In the hydrated and deuterated aluminosilicate and ‐germanate glasses, it is proposed that the degeneracy of the νas(T–O–T) bands is lifted because of structural distortion caused by the presence of H3O+ (D3O+) ions. © 1997 John Wiley & Sons, Ltd.