Stress-modulated surface mass transport offers a possible path to the
ultimate fracture of brittle solids. A positive feedback between the l
ocal geometry, stress concentration, and chemical potential on a rough
surface results in the formation of fracture precursor. Starting from
general kinetic equations, we propose a reduced two-parameter descrip
tion of a growing concavity. A suggested interpolation enables us to o
btain an ordinary differential equation describing the precursor evolu
tion; it starts from a smooth boundary and under certain conditions ge
nerates a cusp singularity. This sharp notch becomes a stress concentr
ator and facilitates direct brittle fracture. The diffusion-limited pr
efracture mechanism, though slow, circumvents a crack nucleation barri
er and can be a determining factor for the durability of materials.