We describe a model for framework silicates in which the SiO4 (and AlO
4) tetrahedra are treated as perfectly rigid and freely jointed. From
this model we are able to identify low-energy modes of distortion of t
he structure, which we call Rigid unit modes. These modes can act as s
oft modes to allow easy distortions at phase transition. We discuss th
ree forces that will operate at a phase transition in conjunction with
the candidate soft modes to determine which of the rigid unit modes w
ill actually precipitate a phase transition, and illustrate these idea
s by detailed discussions of the phase transitions in quartz, leucite
and cristobalite. The model can also be used to estimate the transitio
n temperature, and the theory highlights an important role for the sti
ffness of the tetrahedra.