The boundary conditions on the faces of compressional fractures are not known a priori since these faces may or may not be in contact, but the product of the normal stress and the normal relative displacement is necessarily null; similar but more complex conditions may be written for the shear stress and displacement. These conditions can be expressed in the form of a mixed linear complementarity problem. We use the Displacement Discontinuity Method and the PATH algorithm to solve them. This scheme is faster and more accurate than the methods previously used. The shear stresses on two parallel cracks depend on their separation, their inclination with respect to the imposed maximum compressional stress, and their geometry. The shear stress on two horizontal cracks separated by a small upward or downward step Ð considering the imposed direction of motion Ð drops to zero very near the step; in the case of a downward step this region is surrounded by a small region where the stress increases by a factor of about 10. Many more cases must be investigated before general conclusions can be drawn. 7