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hills
Disequilibrium river networks dissecting the western slope of the Sierra Nevada, California, USA, record significant late Cenozoic tilting and associated surface uplift: Reply
Drainage initiation, expansion, and channel-head arrest in heterogenous bedrock landscapes of the Colorado Plateau
Experimental Evaluation of Water Control for Continuous Packer in Buried Hill Fractured Gas Reservoir: A Case Study of HZ 26-6 Condensate Gas Field
Rainfall Triggering of Post-Fire Debris Flows over a 28-Year Period near El Portal, California, USA
Comparative morphometric analysis suggests ice-cored pingo-shaped landforms on the dwarf planet Ceres
Quantitative analysis of hillshed geomorphology and critical zone function: Raising the hillshed to watershed status
Formation of low-gradient bedrock chutes by dry rockfall on planetary surfaces
Water Saturation Calculation and Fracture Type Identification of a Buried Hill Fractured Reservoir
Late Quaternary geochronologic record of soil formation and erosion: Effects of climate change on Mojave Desert hillslopes (Nevada, USA)
Hydrogeophysical comparison of hillslope critical zone architecture for different geologic substrates
Mitigation of Debris Flows—Research and Practice in Hong Kong
Steep Creek Risk Assessment for Pipeline Design : A Case Study From British Columbia, Canada
The convexity of carbonate hilltops: 36 Cl constraints on denudation and chemical weathering rates and implications for hillslope curvature
Carving Grand Canyon’s inner gorge: A test of steady incision versus rapid knickzone migration
A low-relief hill in eastern Ontario, Canada, covered by the easily erodible Queenston Formation and derived sediments — probably the result of Quaternary tectonic uplift
Shaping post-orogenic landscapes by climate and chemical weathering
Abstract The architecture of the critical zone—the distribution of mobile regolith, the thickness of weathered rock, and their characteristics, as well as the topography of the land surface—is shaped by erosion and weathering processes that depend upon both lithology and climate. In this trip we explore the Boulder Creek watershed, a landscape that juxtaposes uplifted Precambrian crystalline rocks of Colorado’s Front Range against Mesozoic marine sedimentary rocks underpinning the western edge of the High Plains. The landscape is strongly shaped by Quaternary climate cycles operating on this template inherited from the Laramide orogeny. Stop 1 will provide an overview of the abrupt topographic step at the Front Range–High Plains join, where we will discuss fluvial strath terraces on the Plains. At Stop 2 in Betasso Preserve, we will discuss the impact of the canyon cutting set off by late Cenozoic exhumation of the High Plains on the hillslopes and groundwater systems lining the master stream. At Stop 3, we will hike 2 miles down Gordon Gulch, a focus site in the Boulder Creek Critical Zone Observatory. At stops on the hike, we will discuss exhumation rates, climate-modulated weathering, hillslope hydrology and hillslope sediment transport, and the influence of slope aspect on these processes. Our goal is to focus on the history of climate-driven erosion and weathering processes, and how to incorporate these processes into quantitative models of landscape evolution.