The stress state in the subsurface has been shown to be an important parameter for a wide variety of considerations related to seismicity, both natural and anthropogenic. It is characterized for a fault embedded in the subsurface by the shear stress acting along and the total stress acting normal to the plane of the fault. The effective normal stress acting on the fault is then defined as total normal stress minus the contribution of pore pressure. The reactivation of a locked fault is controlled by the ratio of the shear to the effective normal stress acting on the fault plane, as generally dictated by the Mohr-Coulomb criterion. Upon reactivation, slip can either be characterized as seismic or aseismic (i.e., with or without the notable radiation of seismic waves) in nature, depending in large part on the stress state (e.g.,