Supplemental Material: Late Cenozoic deformation in the U.S. southern Colorado Front Range revealed by river profile analysis and fluvial terraces

Text S1: Methods additional information. Figure S1. Slope-drainage area plot for 100 m streamwise distance increments along the eastern Rockies drainage network (grey points) overlain by log-binned averages of the raw data (purple squares). Figure S2: Result from the variance minimization method used to calculate θ_ref=0.41 for the eastern Rockies drainage network. Figure S3: Flexural response of the Arkansas River valley across the western High Plains under T_e = 5 km, 10 km, and 15 km. Table S1: Summary of terrace strath elevations and alluvial fill thicknesses as measured in the field.