  We use a smooth particle hydrodynamics method (SPH) to simulate colliding
rocky and icy bodies from cm-scale to hundreds of km in diameter, in an effort
to define self-consistently the threshold for catastrophic disruption. Unlike
previous efforts, this analysis incorporates the combined effects of material
strength (using a brittle fragmentation model) and self-gravitation, thereby
providing results in the ``strength regime'' and the ``gravity regime'', and in
between. In each case, the structural properties of the largest remnant are
examined.
