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- W1523534444 abstract "[1] Quantifying landscape-scale variations in sediment supply to streams and rivers is fundamental to our understanding of both denudational processes and stream channel morpho-dynamics. Previous studies have linked a variety of sediment-supply proxies to climatic, topographic, or geologic factors, but few have connected these directly to the characteristics of fluvial systems draining these landscapes. Here we correlate landscape controls on sediment supply to observed sedimentology and channel patterns through direct measurements of water and sediment fluxes in over 80 drainage basins ranging in area from 1.4 to 35,000 km2 in the northern Rocky Mountains, USA. These data show that the relative sediment supply, defined by the bankfull sediment concentration, is dominated by basin lithology, while exhibiting little correlation to factors such as relief, mean basin slope, and drainage density. Bankfull sediment concentrations (bed load and suspended load) increase as much as 100-fold as basin lithology becomes dominated by softer sedimentary and volcanic rocks, relative to basins with more resistant lithologies. As bed load concentrations increase, stream beds become less armored, and bed load grain size coarsens. At very high sediment concentrations, bed surface, subsurface, and bed load grain sizes converge and a transition from single-thread to to braided channel patterns is commonly observed." @default.
- W1523534444 created "2016-06-24" @default.
- W1523534444 creator A5009547712 @default.
- W1523534444 creator A5052657378 @default.
- W1523534444 date "2013-11-11" @default.
- W1523534444 modified "2023-10-17" @default.
- W1523534444 title "Sediment supply and channel morphology in mountain river systems: 1. Relative importance of lithology, topography, and climate" @default.
- W1523534444 cites W116612925 @default.
- W1523534444 cites W1486296362 @default.
- W1523534444 cites W1491330286 @default.
- W1523534444 cites W1500881294 @default.
- W1523534444 cites W1517929385 @default.
- W1523534444 cites W1522357428 @default.
- W1523534444 cites W1550788960 @default.
- W1523534444 cites W1565486832 @default.
- W1523534444 cites W1585524865 @default.
- W1523534444 cites W1587869157 @default.
- W1523534444 cites W1936809064 @default.
- W1523534444 cites W1964662062 @default.
- W1523534444 cites W1969970441 @default.
- W1523534444 cites W1970130975 @default.
- W1523534444 cites W1972016282 @default.
- W1523534444 cites W1973024791 @default.
- W1523534444 cites W1974268502 @default.
- W1523534444 cites W1975350041 @default.
- W1523534444 cites W1975711190 @default.
- W1523534444 cites W1977130404 @default.
- W1523534444 cites W1978315128 @default.
- W1523534444 cites W1993265721 @default.
- W1523534444 cites W1993795808 @default.
- W1523534444 cites W1995035032 @default.
- W1523534444 cites W2002606625 @default.
- W1523534444 cites W2003319527 @default.
- W1523534444 cites W2004122326 @default.
- W1523534444 cites W2005252900 @default.
- W1523534444 cites W2007711793 @default.
- W1523534444 cites W2007823307 @default.
- W1523534444 cites W2010481322 @default.
- W1523534444 cites W2011416258 @default.
- W1523534444 cites W2024735597 @default.
- W1523534444 cites W2026886308 @default.
- W1523534444 cites W2027765442 @default.
- W1523534444 cites W2041532132 @default.
- W1523534444 cites W2047168195 @default.
- W1523534444 cites W2049289170 @default.
- W1523534444 cites W2061159032 @default.
- W1523534444 cites W2061491824 @default.
- W1523534444 cites W2067014282 @default.
- W1523534444 cites W2068205597 @default.
- W1523534444 cites W2069646441 @default.
- W1523534444 cites W2070370343 @default.
- W1523534444 cites W2072712492 @default.
- W1523534444 cites W2073772835 @default.
- W1523534444 cites W2074448134 @default.
- W1523534444 cites W2085663892 @default.
- W1523534444 cites W2085666551 @default.
- W1523534444 cites W2088392839 @default.
- W1523534444 cites W2092895365 @default.
- W1523534444 cites W2093570562 @default.
- W1523534444 cites W2095876425 @default.
- W1523534444 cites W2096463624 @default.
- W1523534444 cites W2098797024 @default.
- W1523534444 cites W2101354433 @default.
- W1523534444 cites W2102316187 @default.
- W1523534444 cites W2104292125 @default.
- W1523534444 cites W2106825723 @default.
- W1523534444 cites W2109114408 @default.
- W1523534444 cites W2113974897 @default.
- W1523534444 cites W2115435059 @default.
- W1523534444 cites W2123594378 @default.
- W1523534444 cites W2123631635 @default.
- W1523534444 cites W2126149294 @default.
- W1523534444 cites W2131621559 @default.
- W1523534444 cites W2132394621 @default.
- W1523534444 cites W2132695741 @default.
- W1523534444 cites W2135530338 @default.
- W1523534444 cites W2136012214 @default.
- W1523534444 cites W2141805594 @default.
- W1523534444 cites W2145883138 @default.
- W1523534444 cites W2147000014 @default.
- W1523534444 cites W2157166061 @default.
- W1523534444 cites W2158340899 @default.
- W1523534444 cites W2164751872 @default.
- W1523534444 cites W2167004408 @default.
- W1523534444 cites W2168612292 @default.
- W1523534444 cites W2169938632 @default.
- W1523534444 cites W2270131708 @default.
- W1523534444 cites W2312408544 @default.
- W1523534444 cites W2322314098 @default.
- W1523534444 cites W2346325606 @default.
- W1523534444 cites W2568849 @default.
- W1523534444 cites W4234391467 @default.
- W1523534444 cites W4255637235 @default.
- W1523534444 cites W50436516 @default.
- W1523534444 cites W63943311 @default.
- W1523534444 doi "https://doi.org/10.1002/2013jf002843" @default.
- W1523534444 hasPublicationYear "2013" @default.
- W1523534444 type Work @default.