The article presents the main regularities of the formation of a stone-like fracture of cast steels. The peculiarity of the formation of this defect is the presence of high temperatures and enrichment of the main alloy with small particles and austenitic phases. On the surface of a rock-like fracture, you can often find a matte light gray color, with a metallic sheen. The primary rock-like fracture can be observed after overheating and cooling, that is, before heat treatment. Secondary fracture occurs after metal overheating before hot deformation, such as forging, rolling, and stamping, and also occurs after overheating during heat treatment. The study of patterns of formation of a stone-like fracture in cast steels is one of the most important tasks of modern engineering.