We present a detailed study of a two-dimensional lattice model introduced t
o describe mud cracking in the limit of extremely thin layers. In this mode
l to each bond in the lattice is assigned a (quenched) random breaking thre
shold. Fractures proceed by selecting the 'weakest' part of the material (i
.e. the smallest value of the threshold). A local damage rule is also imple
mented, by using two different types of weakening of the neighbouring sites
, corresponding to different physical situations. We present the results of
numerical simulations on this model. We also derive some analytical result
s through a probabilistic approach known as run time statistics. In particu
lar, we find that the total time to divide the sample scales with the squar
e power L-2 of the linear size L of the lattice. This result is not straigh
tforward since the percolating cluster has a non-trivial fractal dimension.
Furthermore, we present here a formula for the mean weakening of the whole
sample during the evolution.