We present an account of the linear instability of Darcy-Boussinesq convect
ion in a uniform, unstably stratified porous layer at arbitrary inclination
s a from the horizontal. A full numerical solution of the linearized distur
bance equations is given and the detailed graphical results used to motivat
e various asymptotic analyses. A careful study shows that at large Rayleigh
numbers two-dimensional instability can only arise when alpha less than or
equal to 31.30 degrees. However it is also demonstrated that the maximum i
nclination below which this instability may be possible is the slightly gre
ater value of 31.49 degrees which corresponds to a critical Rayleigh number
of 104.30.