Supplemental Material: Transverse faulting in the Paradox Basin, Colorado Plateau, USA: Active, intermittent faulting over a 300 million year history of strain accommodation and fluid flow

This material constitutes a detailed fault-by-fault narrative based on our comprehensive examination of published geologic maps and our own field observations. It includes minimaps for each of the transverse faults and fault zones. Descriptive details are presented in a common order for each fault: general location, primary map reference, nature of faulting, structural association(s), evidence for fault-related channeling of fluid flow, and timing constraints.