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Cq <br />IX <br />7 <br />10 <br />ll <br />0.1 <br />• so <br />f- <br />���� Region 4. Steep braided streams <br />.'p• �: ` ` Region 3. Braided pant -bar and wide -bend <br />pant -bar streams <br />le 0 04 10 7 \ Region 2. Straight !raided streams <br />I 53 \ Region 1. Equiwidth point -bar streams and <br />P4 , 23 320 4 stable canals <br />p — B. surface width in feet 11 D, channel depth in feet <br />° 60 <br />' <br />691 5,15 .0 <br />ri0 ' ,fi B 24 i i \ <br />• o — <br />2 fi� �� Y '� <br />_ ?�4 22 7.65 7 ,' ,h_ i' \ <br />110 •70 i • t25 i 194 _ <br />fo 03 as <br />Sym. Source of data <br />o Schumm <br />• Stable canals } <br />, 192 232 ,� � <br />Miss. river I ,' � - -- <br />�, <br />Number beside a point is No bedload - <br />measured width in feet movement i ; �h• _ _ _ ' <br />n 1n2 Ina 104 105 106 <br />Bankfull discharge, cfs <br />FIGURE A1-5 <br />CHANGE IN CHANNEL MORPHOLOGY <br />RESULTING FROM THRESHOLD <br />REDUCTION IN DISCHARGE <br />Platte River Channel Dynamics Study <br />After Chang (1985). I PARSON 5 Denver, Colorado <br />draxA739921 b.cdr pg t bbs 215102 <br />