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<br />"- <br /> <br />39 <br /> <br />the bends are not reguler and pronounced &II in meande'rir;g teachen.' Even in <br />straight reaches the current tends to wander from one, streubenk to the <br />other. As high flows decrease, suspended solids and bed load deposition <br />occurs forllling bars (i.e., the appearance of small islands at IO~1 flow) <br />opposite from the main current. These barD alternate along the l~nk. .0 <br />that a meandering flow develops in a straight channel at lowH flo.,-,(Figure <br />8). When the streambanks contain large rubble and boulders (i.e., <br />armored), the'.treaa channel tends to be non-erodible, highly st..ble and <br />resistant to the meandering proces.. <br /> <br />PLA.N VIEW <br /> <br />RIFFLE <br /> <br />[ -- -- <br />F~~..l.'..~ <br /> <br />~-..:.:.~ <br />. --- <br />--- - <br /> <br />~::::~ <br /> <br />RIFfLE <br /> <br />RIFFLE <br /> <br />PROF'lLE VIE\.' <br /> <br />/-'''IATER SURFACE <br />. <br /> <br />Il"lFFi.~ <br /> <br />....-... - <br /> <br />-~ <br />; ..I1FL<' <br />. . I ... <br />.., ',......" <br />- ' <br /> <br />POOL <br /> <br />.. ~'iF'FtE'" . <br />. 0' ,.. . <br />....... ~... -r <br /> <br />POOL <br />.:---- <br />. , <br />..--" <br /> <br />-, . <br /> <br />-' <br /> <br />- <br /> <br />-" ~ <br /> <br />STREAMSED-- . <br /> <br />Fll1\1r. R. Pool and riffle fof1Ution In a stt'llltht chann~l (upper). <br />Profile view of humps and depressions fo~ln8 pools and riffles in <br />the .tre.~bed (lower). <br /> <br />Braided Pattern <br /> <br />A braided stream channel is characterized by mult.iple channels that <br />endlessly divide and rejoin (Figure 3). The term anas,tomosis which <br />describes the branching and rejoining of blood vesser; is sometiml!S used to <br />describe the braiding process. The two basJlc characteristics of braided <br />streams are that they have easily eroded stlreambanks .nd that they have <br />more bedload than the stream can transport. As the channel beCOml!S <br />overloaded with sediment, deposition occurs" At low flow, bars form in the <br />widened channel and stabilize to form small islands. This procesll tends to <br />fill the channel and is commonly called .!9udation. In an efforl: to <br />maintain equilibrium the stream gradient increases, velocity inCrl!aSeS, and <br />multiple channels again develop. In areas, lacking st.,bUidng streambank <br />vegetation, the multiple interlaced channels also cause the system to <br /> <br />.,~- <br />