A DEFINITIVE 6 MA START DATE FOR CARVING OF THE NORTHEASTERN COLORADO PLATEAU CANYONLANDS
To date more precisely the onset of incision we present new low-temperature thermochronologic results from bedrock and borehole samples in the northeastern Colorado Plateau. These data show that rapid river incision began here at 6 Ma (5.90±0.59 Ma (2σ) constrained from thermal modeling; 6.0±2.3 Ma (2σ) independently constrained from age-elevation relationship break-in-slope) with incision rates increasing from 15-50 m/Myr to 160-200 m/Myr. This new time constraint has several important implications. First, the coincidence in time with 5.97-5.3 Ma integration of the lower Colorado River through the Grand Canyon to the Gulf of California favors downstream river integration triggering carving of the upper Colorado River canyonlands. Second, it implies integration of the entire Colorado River system in less than 2 million years. Third, rock uplift of the plateau driven by the flexural isostatic response to river incision is restricted to just the last 6 Ma. Fourth, previous estimates of upper Colorado River incision rates based on 10-12 Ma basalt datum levels are too low. This changes the dependency of incision rate on measured time interval from a non-steady-state negative power-law dependence to a near steady-state dependence meaning that long-term upper Colorado river incision rates can provide a reliable proxy for rock uplift rates.