The mesoscopic concept is applied to the description of microcracks. The ba
lance equations of the cracked continuum result in mesoscopic directional b
alances of mass, momentum, angular momentum, and energy. Averaging over the
length of the cracks gives the corresponding orientational balances. A fur
ther averaging process leads to the macroscopic balance equations of the mi
crocracked continua. Dynamic equations for the fabric tensors of different
order are derived using a multipole moment expansion of the orientational c
rack distribution function. The simple example of Griffith cracks is treate
d. The role of physical assumptions in the microcrack representations and t
he different macroscopic internal variable representations of microcracks a
re discussed.