By employing the adaptive network simulation method, we demonstrate that th
e ensemble-averaged stress caused by a local force for packings of friction
less rigid beads is concentrated along rays whose slope is consistent with
unity: forces propagate along lines at 45 degrees to the horizontal or vert
ical. This slope is shown to be independent of polydispersity or the degree
to which the system is sheared. Further confirmation of this result comes
from fitting the components of the stress tensor to the null stress "consti
tutive equation". The magnitude of the response is also shown to fall off w
ith the -1/2 power of distance. We argue that our findings are a natural co
nsequence of a system that preserves its volume under small perturbations.