Griffith proposed that brittle materials contain small cracks and flaws that concentrate stress enough to reach the theoretical strength at nominal stresses below theoretical values. For a crack to propagate, the decrease in elastic strain energy from crack growth must be equal to or greater than the increase in surface energy. Griffith established a criterion where the stress required for crack propagation is inversely proportional to the square root of the crack length. This theory provides an equation to calculate the maximum crack length possible without fracture given a material's surface energy, modulus of elasticity, and applied stress.