The dynamics of a crack propagating in an elastic inhomogeneous material is investigated. The variations of the average crack velocity with the external loading are measured for a brittle rock and are shown to display two distinct regimes: Below a given threshold Gc, the crack velocity is well described by an exponential law v ≃ e − C G− Γ characteristic of subcritical propagation, while for larger values of the driving force G > Gc, the velocity evolves as a power law v ≃ (G − Gc) θ with θ = 0.80 ± 0.15. These results can be explained extending the continuum theory of Fracture Mechanics to disordered systems. In this description, the motion of a crack is analogue to the one of an elastic line driven in a random medium and critical failure occurs when the loading is sufficiently large to depinne the crack front from the heterogeneities of the material.PACS numbers: 62.20. Mk, 46.50.+a, 68.35.Ct Failure of inhomogeneous materials has been a very active field of research during the last decades (see Ref.[1] for a recent review). A great research effort in this field has been dedicated to the study of fluctuations: Fluctuations of velocity around the average motion of cracks when the studies were devoted to their highly intermittent dynamics [2,3,4,5], or variations to a straight trajectory when the works were dedicated to the rough geometry of fracture surfaces [6,7,8]. In both cases, these fluctuations were shown to display remarkably robust properties suggesting that crack propagation in disordered systems could be described on a general manner by relatively simple statistical models able to capture the competition between the two antagonist effects occurring during failure of inhomogeneous materials: Disorder and elasticity.Very recently, main statistical features of fluctuations of both trajectory and velocity for cracks propagating in brittle materials were captured by stochastic models of elastic lines driven in random media [9,10] that mimic the motion of cracks through the microstructural disorder of materials. However, the relevance of this theoretical framework for fracture problems is still a matter of debate: On the one hand, the ability of these models to describe the average behavior of the crack such as its mean velocity, or the critical external loading at failure, more interesting from a mechanical or an engineering point of view, is still an open question. On the other hand, a direct experimental observation of the critical dynamic transition from a crack pinned by the heterogeneities of the material (v = 0) to a propagating crack (v > 0), as predicted by this theory at the onset of material failure (driving force G = G c ), is still lacking. The investigation of this depinning transition on an experimental example is the central point of this Letter.The variations of the average crack velocity with the external driving force, i.e. the energy release rate G [11], are measured for a brittle rock. They are shown to exhibit two distinct regimes. Below a critical threshold G c , the crack velocity...