Abstract. One of the unanswered questions in the study of fatigue is how cracks nucleate at stresses far below the static fracture strength. Previous theories show possible qualitative mechanisms that may operate in a crystal at room and low temperatures but none provides a quantitiative theory of this phenomenon. We show here a quantitative mechanism of fatigue crack initiation.With a small initial stress field, two closely located thin slices slide in opposite directions under cyclic loading. The increase of the local plastic strain with cycles of loading is calculated. The local plastic shear strain, positive in one slice and negative in the other, reaches 100 per cent at the free surface in a few hundred cycles. These large strains clearly cause the start of an extrusion or intrusion and fatigue crack nucleation.Answers to the question of how fatigue cracks nucleate in metals under stresses far below the static fracture strength have been sought by many investigators since the beginning of the century. However, this question is far from having been clearly answered. In this paper, we attempt to answer it by showing a nucleation mechanism and a method to determine quantitatively the local plastic strain under cyclic loading.The development of the present mechanism of fatigue crack nucleation is guided by the following experimental observations.1-4 The observed fatigue in metals down to 1.70K indicates that surface corrosion, gas adsorption, or vacancy diffusion is not necessary to the nucleation mechanism. The formation of fatigue cracks is associated with slip, and slip lines appear at early stages of fatigue. As the number of loading cycles increases, these slip lines broaden into bands in which fatigue cracks ultimately form. Reverse loading produces slip lines which are close to, but not coincident with, the slip lines formed in the forward loading. This indicates that two distinct, very closely located, sliding slices intersect the free surface. One slice slides during the forward loading, producing one slip line, and the neighboring slice slides during the reverse loading, producing the other slip line.Tests have shown that single crystals, under high stress, slide along certain directions on certain crystallographic planes and that the slip depends on the shear stress along the slip direction on the slip plane (called the resolved shear stress of this slip system) and is independent of the normal pressure on the sliding plane.5 The resolved shear stress that initiates or causes further slip is known as the critical shear stress. This dependency of slip on the resolved shear stress is applied to the present analysis.Lattice imperfections exist in all metals and produce an initial heterogeneous stress field. Certain small initial stress fields can cause the above sequence 631