Schubert G, Lingenfelter RE, Peale SJ (1970) The morphology, distribution, and origin of lunar sinuous rilles. Richards KS (1982) Rivers: form and process in alluvial channels. Reading HG (1996) Sedimentary environments, 3rd edn. In: Goudie AS (ed) Encyclopaedia of geomorphology. Marani M, Lanzoni S, Zandolin D, Seminara G, Rinaldo A (2002) Tidal meanders. 42nd Lunar Planet Sci Conf, abstract #1562, Houston Malaska M, Radebaugh J, Le Gall A, Mitchell K, Lopes R, Wall S (2011) High-volume meandering channels in Titan’s south polar region. Luchi R, Bolla Pittaluga M, Seminara G (2012) Spatial width oscillations in meandering rivers at equilibrium. In: Gregory KJ (ed) River channel changes. Lewin J, Brindle BJ (1977) Confined meanders. Geological Survey professional papers 282. Leopold LB, Wolman MG (1957b) River channel pattern: braided, meandering and straight. US Geological Survey professional paper 282-C. Leopold LB, Wolman MG (1957a) River flood plains, some observations on their formation. US Geological Survey professional paper, 422-H. Langbein WB, Leopold LB (1966) River meanders-theory of minimum variance. Transportation Research Board, Washington, DC ![]() Lagasse PF, Spitz WJ, Zevenbergen LW, Zachimann DW et al (2004) Handbook for predicting stream meander migration. Komatsu G, Baker VR (1994) Meander properties of Venusian channels. Knighton AD (1998) Fluvial forms and processes, 2nd edn. 6th International conference on Mars, #3039 Kereszturi A (2003) Paleodischarge estimation from morphometry for ancient channels. Karlstrom L, Gajjar P, Manga M (2013) Meander formation in supraglacial streams. Kargel JS, Kirk RL, Fegly B Jr, Treiman AH (1994) Carbonatesulfate volcanism on Venus? Icarus 112:219–252 42nd Lunar Planet Sci Conf, abstract #2748, Houston Irwin RP (2011) Timing, duration, and hydrology of the Eberswalde crater paleolake, Mars. Hudson PF, Kesel RH (2000) Channel migration and meander-bend curvature in the lower Mississippi River prior to major human modification. Howard ADH (2009) How to make a meandering river. Lunar Planet Sci XXXVIII, abstract #1226, Houstonįryirs KA, Brierley GJ (2012) Geomorphic analysis of river systems: an approach to reading the landscape. doi:10.1130/B30612.1ĭe Hon RA (2007) On meanders and sinuosity of Martian channels. doi:10.1029/2009JE003496īurr DM, Perron JT, Lamb MP, Irwin RP III, Collins GC, Howard AD, Sklar LS, Moore JM, Ádámkovics M, Baker VR, Drummond SA, Black BA (2012) Fluvial features on Titan: insights from morphology and modeling. Wiley, Chichester, UKīurr DM, Williams RME, Wendell KD, Chojnacki M, Emery JP (2010) Inverted fluvial features in the Aeolis/Zephyria Plana region, Mars: formation mechanism and initial paleodischarge estimates. ![]() 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.
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |