Tempe Terra is a structurally complex region situated at the northeast edge of the Tharsis Rise volcano-tectonic province (Figure 1). Crustal stresses associated with the development of the Tharsis Rise resulted in the formation of radial extensional features and concentric shortening features surrounding Tharsis (Figure 1) (Anderson et al., 2001). Despite decades of research into various aspects of the Tharsis Rise (e.g.,