Sharp Lecture: EP32A. Bedrock Hillslopes to Deltas: New Insights into Landscape Mechanics

• Report rights infringement
• published: 06 Dec 2012
• views: 312

Sharp Lecture: EP32A. Bedrock Hillslopes to Deltas: New Insights into Landscape Mechanics - 2012 AGU Fall Meeting Abstract: http://abstractsearch.agu.org/meetings/2012/FM/EP32A-01.html A powerful record of environmental history on Earth and other planets is preserved in landscapes and sedimentary deposits formed by erosion, transport and deposition of sediment. To understand this record and predict future landscape change, we need mechanistic theories for transport processes and morphodynamics. Significant progress has been made to develop and test transport laws in some settings including soil-mantled landscapes and modest gradient alluvial channels where conventional hydraulic and sediment-transport theories apply. Fundamental opportunities exist, however, to explore the physical limits of existing theories and develop new theories at the frontier of our knowledge base. In this presentation, I will describe recent case studies from sediment-source areas to depositional sinks designed to test the limits of existing transport theories and identify transitions in dominant geomorphic processes by pushing to steeper slopes, greater discharges, and dynamic boundary conditions. First, field measurements, laboratory experiments and theory suggest that sediment transport on steep, rocky hillslopes is different than on soil mantled landscapes, and may be controlled by vegetation dams and sediment release following wildfire. Second, laboratory experiments show that grain stability is enhanced in steep mountain channels compared to moderate gradient channels due to the coincident change in the ratio of flow depth to grain size, until the threshold for mass failure is surpassed. Third, field observations and theory indicate that canyons can be cut by extreme floods at rates that exceed typical river-incision rates by many orders of magnitude due to the transition from abrasion to plucking and toppling of jointed rock, with implications for megafloods on Mars. Finally, numerical modeling, laboratory experiments, and field work show that coastal rivers are coupled to their offshore plumes, and that this coupling may determine the size of deltas. These case studies illustrate that relevant processes, from turbulence to tectonics, act over a wide range of spatial and temporal scales. A major future opportunity I see is to integrate topographic and geochronologic constraints on landscape kinematics with field and laboratory experiments on process dynamics to build mechanistic transport theories applicable across human and geomorphic timescales. Cite as: Author(s) (2012), Title, Abstract EP32A-01 presented at 2012 Fall Meeting, AGU, San Francisco, Calif., 3-7 Dec.