LEADER 01707oam 2200505 450 001 9910706552703321 005 20171130093611.0 035 $a(CKB)5470000002456920 035 $a(OCoLC)965753625$z(OCoLC)892425224 035 $a(OCoLC)995470000002456920 035 $a(EXLCZ)995470000002456920 100 $a20161210d1961 ua 0 101 0 $aeng 135 $aurmn||||||||| 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 14$aThe shape of alluvial channels in relation to sediment type /$fby S. A. Schumm 210 1$aWashington :$cUnited States Department of the Interior, Geological Survey,$d1960. 215 $a1 online resource (23 unnumbered pages) $cillustrations 225 1 $aGeological Survey professional paper ;$v352-B 300 $a"Erosion and sedimentation in a semiarid environment." 320 $aIncludes bibliographical references (page 30). 606 $aRiver sediments 606 $aChannels (Hydraulic engineering) 606 $aAlluvial streams 606 $aHydraulic engineering 606 $aHydraulic engineering$2fast 615 0$aRiver sediments. 615 0$aChannels (Hydraulic engineering) 615 0$aAlluvial streams. 615 0$aHydraulic engineering. 615 7$aHydraulic engineering. 700 $aSchumm$b Stanley A$g(Stanley Alfred),$f1927-2011,$01395981 712 02$aGeological Survey (U.S.), 801 0$bOCLCE 801 1$bOCLCE 801 2$bOCLCQ 801 2$bCOP 801 2$bOCLCF 801 2$bGPO 906 $aBOOK 912 $a9910706552703321 996 $aThe shape of alluvial channels in relation to sediment type$93455316 997 $aUNINA