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Landscape disturbance events (e.g., earthquakes, slope failures) play key roles in landscape evolution in tectonically active areas. Along the Teton fault, fault scarps vary in height by up to tens of meters. LiDAR-based mapping indicates that scarp height is affected by glacial geomorphology, slope failure, and alluvial processes. LiDAR data, digital and field mapping were used to characterize fault scarps and slope failure deposits along the Teton fault zone. Based on vertical separation (VS; the vertical offset between faulted surfaces) across fault scarps and the expected behavior of normal faults, we propose a four-section model of the Teton fault. At a broad scale, VS is greatest along the southern fault zone. At a finer scale, VS is least at the ends of the fault and at three areas within the central fault zone. Transitions between these four sections may represent segment boundaries with potentially important implications for geohazards assessment.