Meander belts7/4/2023 Reston, VA, 77-43īrierley GJ, Fryirs KA (2005) Geomorphology and river management: applications of the River Styles framework. Geological Survey, Water-Resources Investigations. doi:10.1029/2006JE002785īrice JC (1977) Lateral migration of the middle Sacramento River, California. J Sediment Res 80:852–866īray VJ, Bussey DBJ, Ghail RC, Jones AP, Pickering KT (2007) Meander geometry of Venusian canali: constraints on flow regime and formation time. Elsevier, Amsterdamīarbonneau N, Savoye B, Cremer M, Bez M (2000) Sedimentary architecture in meanders of a submarine channel: detailed study of the present Congo turbidite channel (Zaiango project). This process is experimental and the keywords may be updated as the learning algorithm improves.Īllen JRL (1982) Sedimentary structures: their character and physical basis II. These keywords were added by machine and not by the authors. 49) or, alternatively, the zone between tangents to the outsides of the curves or meanders of the active stream (Allen 1982, p. The meander belt is “the zone of active and recently abandoned channels and their adjacent overbank environments” (Reading 1996, p. Riffles or crossings develop at the inflexion points pools develop at the bend apex (Fig. Meandering point bar rivers generally show maximum width at bend apexes, in contrast to sinuous canaliform rivers which has maximum width at inflection points (Luchi et al. Meandering and sinuous rivers generally display spatial oscillations of their width. ![]() Leopold and Wolman ( 1957b) selected the arbitrary sinuosity value of 1.5 to distinguish between meandering channels (sinuosity >1.5) and sinuous (sinuosity <1.5) or straight channels.
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