The equations of motion for 'rapid' flow of a granular material have f
ully developed solutions representing flow driven by a body force, suc
h as gravity, along a channel bounded by plane parallel walls. The sta
bility of these solutions to small perturbations is investigated. For
given properties of the particles and the channel walls it is found th
at the condition of critical stability is a relation between the mean
concentration of the particles and the width of the channel. When the
base state is unstable the fastest growing modes are travelling waves
propagating in the axial direction and these induce characteristic pat
terns of variations in particle concentration, as well as velocity. Th
ese instabilities are contrasted with those found for Couette shearing
in an earlier publication.