This document summarizes Griffith and Irwin fracture mechanics theories. [1] Griffith's theory explains brittle fracture and proposes that crack growth occurs when the potential energy released by fracturing exceeds the new surface energy. [2] Irwin modified Griffith's theory for ductile materials by including a term for the energy dissipated by plastic deformation near the crack tip. Irwin's theory partitions the energy into stored elastic energy driving fracture and dissipated energy resisting it. Crack growth occurs when the stored energy exceeds the dissipated energy.