“…Discontinuities happen to be often the weak points of rock materials, since, if movements in the rock mass occur, it tends to happen along these surfaces. The point where the initiation of the movement along the surfaces takes place, depends on the shear strength along the discontinuities, and therefore their investigation is one of the most important topics in rock mechanics [1,2,3]. The shear strength of rocks along discontinuities is influenced by several factors, for example, surface roughness of the joint, joint infill material, elevation of the plane of the sample surface in respect to the shear plane in the direction of shear, rock strength, normal stress acting on the sample surface, humidity, bedding, and in situ stress conditions...etc [4,5,6,7,8,9].…”