The infrared spectra of the entire glass-forming range of the vitreous system Mo-P-O are reported. The data are interpreted in the light of previous studies of other vitreous phosphates, and related crystalline phosphates. The spectra show that with increasing MoO 3 content progressive rupture of P = O bonds takes place and there is little of the bond-type left in compositions exceeding 53 mol% MoO 3 . The P=88O stretching frequency is reduced by hydrogen bonding but increases with increasing Mo content. The P-O-P ring frequency is strong throughout most of the composition range, consistent with a three-dimensional network structure relatively free of chains. The spectra in midcomposition range are characterised by vibrations characteristic of PO 3 and P 2 O 7 groups with edge sharing MoO 6 octahedra having relatively little effect. However, the spectra of Morich structures display unique features characteristic of edge sharing MoO 6 octahedra as in pure MoO 3 oxide. Generally, the data are also consistent with the proposition, used in a previous ultrasonic study, that these glasses consist of distorted versions of the crystal groups: PO 4 tetrahedra, MoO 3 octahedra, metaphosphate and pyrophosphate, in proportions that change systematically and distinctively with content. It is suggested that acoustic and optical Debye temperatures calculated from these spectra ought to correlate with (in respect of composition dependence) analogous quantities calculated from published data on acoustic wave velocities and the temperature dependence of electrical conductivity in this wide-ranging glass system.