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

journal contribution
posted on 2023-05-03, 15:06 authored by Eyal Marder, et al.

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.