DYNAMIC RIVER SYSTEMS IN THE GRAND STAIRCASE, SOUTHERN UTAH: THE ROLE OF HIGH EROSION RATES, HYDROCLIMATE VARIABILITY AND GEOMORPHIC THRESHOLDS IN HOLOCENE ARROYO DYNAMICS (Invited Presentation)
This presentation reports on the geomorphology and chronostratigraphy of five catchments draining the Grand Staircase in southern Utah. Age control used to constrain arroyo cut-fill sequences (n= 70 sites) comes from radiocarbon dating of charcoal (n=180) and single-grain optically stimulated luminescence dating (n=140). Catchment-averaged erosions rates come from Be-10 cosmogenic radionuclide (CRN) concentrations in modern, Holocene and Pleistocene sediments (n = 65).
Reconstructions indicate that each catchment had 3-5 periods of aggradation followed by entrenchment, with the timing of events most similar in the last 2-3 ka. CRN results indicate high bedrock erosion rates, which fueled high sediment supply and largely aggradational Holocene conditions across the region. Following aggradation, stream profiles had reduced concavity and locally over-steepened downstream reaches, which provided the necessary gradients to drive entrenchment. However, the timing of arroyo cutting was ultimately controlled by 1) sediment supply and the time it takes a catchment to aggrade and reach a concavity-slope driven threshold and 2) hydroclimatic variability, as the driving forces for entrenchment only occurred during high-discharge events once aggradation brought the systems to a threshold in slope. A conceptual model is presented to illustrate how hydroclimatic variability, geomorphic thresholds and catchment specific relaxation/recovery time combined to produce the quasi-synchronous nature of the regional arroyo cut-fill records.