Heat or mass transfer across crack surfaces can generate localized shrinkag
e causing internal stresses which drive crack propagation. We present exper
iments suggesting the existence of such a diffusion controlled directional
self-cracking. Ne formulate a simple two-dimensional stationary model of st
raight, evenly spaced, parallel cracks for this process, which takes into a
ccount the heat transfer across the crack surfaces and the interaction of n
eighboring cracks. The governing equations are solved numerically using fin
ite elements. Crack spacing and velocity can be predicted utilizing a stabi
lity argument combined with simple ideas about the formation of the crack a
rray. The selected solution is marginally stable with minimal values for cr
ack spacing and velocity. The results are compared with predictions from a
simpler model by Yakobson.