We study the approach to global breakdown in disordered media driven b
y increasing external forces. We first analyze the problem by mean-fie
ld theory, showing that the failure process can be described as a firs
t-order phase transition, similarly to the case of thermally activated
fracture in homogeneous media. Then we quantitatively confirm the pre
dictions of the mean-field theory using numerical simulations of discr
ete models. Widely distributed avalanches and the corresponding mean-f
ield scaling are explained by the long-range nature of elastic interac
tions. We discuss the analogy of our results to driven disordered firs
t-order transitions and spinodal nucleation in magnetic systems.