We consider the boundary layer that forms on the wall of a relating contain
er of stratified fluid when altered from an initial state of rigid body rot
ation. The container is taken to have a simple axisymmetric form with slopi
ng walls. The introduction of a non-normal component of buoyancy into the v
elocity boundary-layer is shown to have a considerable effect for certain g
eometries. We introduce a similarity-type solution and solve the resulting
unsteady boundary-layer equations numerically for three distinct classes of
container geometry. Computational and asymptotic results are presented for
a number of parameter values. By mapping the parameter space we show that
the system may evolve to either a steady state, a double-structured growing
boundary-layer or a finite-time breakdown depending on the container type,
rotation change and stratification. In addition to extending the results o
f Duck et al. (1997) to a more general container shape, we present evidence
of a new finite-time breakdown associated with higher Schmidt numbers.