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River Form is a Function of: <br />• Discharge (Peak Flow) <br />• Sediment Supply <br />• Vegetation <br />• Sediment Grain Size <br />• Channel Slope <br />. = = = = == Interaction of Above <br />Construction of large <br />reservoirs and diversion of <br />flows: <br />• PhysicallyTraps sediment. <br />• Stores peak flows. <br />• Sed. transport: Was about 7 - 8 million tons /year <br />• Now about 1 million tons /year <br />• Shifted the primary sediment source from <br />the North Platte River (finer grain size) to <br />the South Platte River (coarser grain size). <br />5 <br />