Compare and contrast how the Sandy River s active channel width and floodplain width changes as you travel downstream from the

Question

Compare and contrast how the Sandy River s active channel width and floodplain width changes as you travel downstream from the Sediment Source Reach to the start of the Response Reach The Sediment Source Reach is the area that is the source of the sediment I e the upstream location In the image below the water is running from the top of the image down to the bottom of the image So the Sediment Source Reach is the area at the top of the image and the Response Reach is the downstream location located at the bottom of the image The diagram below shows what the active channel and floodplain looks like channel cutoff natural levee bedrock bar swale topography point bar incipient oxbow alluvium floodplain Ameander scars yazoo stream oxbow lake

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