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Facet-like morphologies were found in both the fatigue crack origin and growth regions; however, their microscopic features were different. Smooth features implying single-slip deformation were observed at the origin, while characteristic regular triangular and tetrahedral configurations, reflecting {1 1 1} planes and indicating multiple-slip deformation, were observed at the growth region. Some unique morphological features were found in the tensile fracture region following the fatigue fracture region. These distinct microscopic features might indicate the fracture of annealing twin boundaries. Other features on the surface of the primary epsilon-martensite variant from collision with the secondary epsilon-martensite variant were also recognized. 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