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River morphology and process class 1. consider physics of flow and erosion 2. review river taxonomy 3. examine the germane processes that control the shape of river channels 4. consider the graded profile 5. consider the impact of floods and tectonic setting on river channels Gravity = driving force Solar = energy source • Gravity responsible for movement of water down gradient, PE = mgh ~ h • Precipitation maintains supply of fluid, driven by solar forcing • Tectonics maintains gradient, driven by erosion and endogenic forces • Consider fluid forces acting on sediment, critical shear stress (crit, need to detach grains • Balance of erosion, sediment supply shapes channels 1 Hujlstom Diagram 1 1 MODES OF SEDIMENT TRANSPORT • Sliding • Rolling • Saltation • SHOW FLASH MOVIE QuickTime™ and a Sorenson Video decompressor are needed to see this picture. Taxomony QuickTime™ and a TIFF (Uncompressed) decompressor are needed to see this picture. 2 Downstream Organization 2 Channel Mobility Watts Branch, MD 2/3 Flow is not uniform in plan view 3 Water velocity is not uniform with depth Consider friction and laminar flow; mean velocity at 0.6 d Idealized flow patterns Dye tracing Alluvial, meandering river 3 Graded profile, idealized form • rivers will try and adjust to minimize energy gradient • tectonics and climate change get in the way Can the river keep up? •Gorges reflect cutting •Knick zones reflect inability to cut quickly enough QuickTime™ and TIFF (Uncompressed) dec a omp are needed to see this pictu ressor re. Taiwan What does climate change do? QuickTime™ and a TIFF (Uncompressed) decompressor are needed to see this picture. QuickTime™ and a TIFF (Uncompressed) decompressor are needed to see this picture. QuickTime™ and a TIFF (Uncompressed) decompressor are needed to see this picture. Glacial hanging valleys, bedrock channel erosion Gaysville before the flood QuickTime™ and a TIFF (Uncompressed) decompressor are needed to see this picture. 1927 flood - Gaysville, VT - after