By molecular-dynamics simulations, we have studied the devitrification (or crystallization) of aged hard-sphere glasses. First, we find that the dynamics of the particles are intermittent: Quiescent periods, when the particles simply "rattle" in their nearest-neighbor cages, are interrupted by abrupt "avalanches," where a subset of particles undergo large rearrangements. Second, we find that crystallization is associated with these avalanches but that the connection is not straightforward. The amount of crystal in the system increases during an avalanche, but most of the particles that become crystalline are different from those involved in the avalanche. Third, the occurrence of the avalanches is a largely stochastic process. Randomizing the velocities of the particles at any time during the simulation leads to a different subsequent series of avalanches. The spatial distribution of avalanching particles appears random, although correlations are found among avalanche initiation events. By contrast, we find that crystallization tends to take place in regions that already show incipient local order.colloidal glasses | ordered solid | amorphous solid | dynamic heterogeneities G lasses are formed from the supercooled liquid state when motion is arrested on the scale of the particle diameter. Such states are thermodynamically unstable and may crystallize during, or shortly after, the initial quench. (This is the usual fate of so-called "poor" glass formers.)Computer simulations have shown that, in such cases, crystallization readily proceeds by a sequence of stochastic micronucleation events that enhance the mobility in neighboring areas, leading to a positive feedback for further crystallization (1). Importantly, however, crystallization can also arise in mature, well-formed glasses after a long period of apparent stability. The microscopic mechanism of this process, known as "devitrification," remains elusive. Here, we simulate the dynamics of a mature hard-sphere glass and find that crystallization is associated with a series of discrete avalanche-like events characterized by a spatiotemporal burst of particle displacements on a subdiameter scale. The locations of these avalanches cannot be predicted from the prior structure of the glass, and they vary among replicate runs that differ only in initial particle velocities. Each avalanche leads to a sharp increase in crystallinity, but remarkably the crystallizing particles are primarily not those that participated in the avalanche itself. Instead, they tend to lie in nearby regions that are already partially ordered. We argue that a structural propensity to crystallize in these regions is converted into actual crystallinity by small random disturbances provided by the displacement avalanche. Although spontaneous rather than externally imposed, this pathway may relate to designed crystallization protocols such as oscillatory shear.Devitrification is a phenomenon of both fundamental interest (2, 3) and practical importance (4-10). Indeed, the prediction and avoidance...