“…Long recurrence intervals involving disparate fault arrays on timescales of several 10 3 years can result in obliteration and overprinting of rupture traces, due to postseismic sedimentation, erosion [e.g., Scholz , ], and anthropogenic activity [e.g., Landgraf et al , ], rendering a rigorous determination of fault activity and hazard assessment difficult. As a result, damage and losses are often substantially higher than in plate boundary areas, where the higher frequency of earthquakes generally results in better preparedness [e.g., England and Jackson , ; Dengler et al , ]. This dilemma is furthermore exacerbated by rapid urbanization, growing population, and the concentration of economic values in many continental interiors that have been affected by infrequent earthquakes [e.g., Bilham , ].…”