chapter 3 fundamentals of fluvial geomorphology and stream ...

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aiding. Braid bars are sediment features found between thesub-streams of multi-thread, braided rivers (Figure 3.7b). Braidbars are highly mobile, and deflection of flow due to bar movementis responsible for the shifting pattern of anabranches and frequentbank attack that characterize braided-river morphology.Figure 3.5 – Typical MeanderingStream with Point BarsFigure 3.6 – Typical Middle Bar28 Fundamentals of Fluvial Geomorphology and Stream Processes
(a) AlternateFigure 3.7 – Typical Bar Patterns(b) BraidedFundamentals of Fluvial Geomorphology and Stream Processes 29
Page 6 and 7: materials. Also, the threshold mobi
Page 8 and 9: ank of a large river. From an engin
Page 10 and 11: eddies in a stream do not scale on
Page 14 and 15: Sinuosity (P) is a commonly used pa
Page 16 and 17: outcrops, other non-erodible materi
Page 18 and 19: continent (Inglis 1941, 1947, 1949)
Page 20 and 21: instances where the bankfull discha
Page 22 and 23: uses readily available mean daily f
Page 24 and 25: of flows. The results are plotted a
Page 26 and 27: Similarly, in regime theory the con
Page 28 and 29: 3.7 STREAM STABILITY ANDINSTABILITY
Page 30 and 31: It should be noted that the map coo
Page 32 and 33: and slope of the reach are not sign
Page 34 and 35: (a) Bed and Bank InstabilityFigure
Page 36 and 37: the downstream limit of the system
Page 38 and 39: dam, where degradation was expected
Page 40 and 41: Figure 3.13 - Channel PatternClassi
Page 42 and 43: definition of a graded stream in wh
Page 44 and 45: midwestern experience, while Rosgen
Page 46 and 47: Schumm et al. (1981, 1984) and thei
Page 48 and 49: ut at a much reduced rate. The sedi
Page 50 and 51: • integration of results into eng
Page 52: 68 Fundamentals of Fluvial Geomorph

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