Fractures are ubiquitous in the Earth's crust. They strongly impact the mechanical stability, strength, and permeability of geological structures or rock masses and thereby play an essential role in many societally important processes in the upper crust as well as in the management of subsurface engineering operations. The most common are the so-called opening mode (extension or tensile/tension) fractures or joints. They often form regular sets of parallel, orthogonal, or more complex fracture networks. Because of their practical importance, notably for the oil and gas industry, joints have been extensively studied for more than a century (e.g., Pollard & Aydin, 1988), mostly in sedimentary basins composed of alternating layers with contrasted lithology (Figures 1a-1c) and hence mechanical properties. Particular attention has been paid to the joint spacing S or the ratio D of the fractured layer thickness T to S (D=T/S). The main practical aim has been to predict the fracture spacing at depth from bed thickness. The spacing of natural fractures cannot be observed directly in the subsurface, whereas the bed thickness can be defined from petrophysical well data or core analysis. These works stimulated research in rock/fracture mechanics and modeling