Based on this map of the flood path, between Red Rock Pass and Pocatello, explain the occurrence of flood deposits based on the channel geometry and how channel geometry affects basal shear stress and stream power. Assume that water discharge does not change through this reach. The Impact of Channel Geometry on Flood Deposits Between Red Rock Pass and Pocatello

Channel Geometry and Flood Deposits: The Effect of Channel Geometry Between Red Rock Pass & Pocatello
This map shows the flood path connecting Red Rock Pass with Pocatello. The channel has a variable geometry. In the western portion, it is narrow and sinuous while in the eastern part, it’s wide and winding. The occurrence of flood deposit in this area is directly affected by the variable geometry. With the channel becoming wider, basal shear stresses decrease and stream power decrease (Smith, 2017; Lane, 2019). The river’s ability to transport sediment is affected by this decrease. Flood deposits can result from the deposition of sediment. However, in more sinuous sections the channel becomes narrower, and the basal shear stresses increase, leading to an increase in stream power (Lane 2019). This increases stream power allows the river to move more sediment, which results in deposition rather than scouring. It is because of this that there are not flood deposits at the sinuous areas, as shown on the map. Cont…
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