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While it is true that the term crack is often taken to mean what it was originally intended to, i.e. a weak area in a solid, in this case the term is incorrectly used to mean a weak spot in the otherwise strong (infinite) inter-molecular bonds of a crystal. In this case, crack means a weak area in a solid. For this reason, despite its being a relatively common use, the correct use of this term is discouraged.
Crack propagation in solids is a phenomenon of great importance in a number of technical fields. In this paper, we present results from the propagation of cracks in a natural rock. Observations were made of the propagation of cracks in a rock in a laboratory. The observations were made using a high-speed photography system. The rock was loaded with water in such a way that it was stretched apart by a force applied at one end. The load was progressively increased until the rock failed, and the crack length at the rock failure was determined.
For engineering materials, we investigate the potential for using Mohr-Coulomb (or equivalent) stress-crack-propagation mechanisms as an aid to the analysis of fracture. Our investigation is based on the material of the vast proportions of the United States.
For the past 50 years, the term crack has been used interchangeably with flaw, in one sense, to mean a type of stress concentration, and in another sense to mean a fracture in a brittle material. We present a definition for crack as a split of the material that is not intentional. According to this definition, a crack is essentially an infinitesimal split in the material. A crack may start anywhere on the surface. As long as it does not affect the integrity of the material, it is usually ignored, but when it does, it may have an adverse effect on the properties of the material. A crack propagates in a brittle material by splitting the material into two or more pieces. A crack is oriented on the direction of the highest stress that is being applied to the material.
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