It has always been assumed that basal dislocations are the main deformation micromechanism operative when layered crystalline materials are loaded in compression. Recently, the authors showed that ripplocations, small ripples in the layers, and not basal dislocations are the operative mechanism. Herein, by modeling the indentation of graphite, using atomistic methods, the authors show that the ripplocation nucleation stresses are dependent on the strain gradients engendered by the different indenter radii modeled. Furthermore, they show how the rapid alignment of ripplocations, on adjacent layers, form oppositely oriented ripplocation boundaries that quickly propagate—wavelike—away from just below the indenter. This massive strain delocalization has never been previously reported in contact mechanics where it has always been assumed that the range of influence of an indenter was roughly the size of the indenter.