We discuss the stress relaxation in a uniaxially strained solid due to the
coarsening of a system of parallel cracks. We emphasize similarities and di
fferences of this process to Ostwald ripening in a first order phase transi
tion. A conventional mean-field approximation breaks down and several indep
endent length scales have to be taken into account. Strong elastic interact
ions between the cracks determine the growth behavior. We derive scaling la
ws for the coarsening of the different length scales involved and the time
evolution of stress relaxation, finally leading to the equilibrium state of
a fractured body. The characteristic size of the cracks grows linearly in
time which is much faster than in usual Ostwald ripening.