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appropriate basis Bed Equilibrium Computed bed load dragged bottom equilibrium Carpathian rivers channel characterized CM CM CM CM O O considerable continuous line Course of Slopes curve of consecutive curve of sifting debris degree of development determining G0 diagram differences dotted lines dragging force drawn Dunajec San Dynamic Factors established f(so factors indicated Factors of River formula fractions function Go functional correlation given cross section given gravel mixture grain-size graphical form gravel grains horizontal investigate the correlation Kajetanowicz kilometer km i Go length located longitudinal profile magnitude Mean depth modulus MOUNTAIN RIVER BED parabolas smoothing petrographical physiographical factor plotted point of intersection Raba river basin River Bed Equilibrium RIVER BED LOAD river bottom river investigated samples scattering shape smoothed slopes smoothing the longitudinal sq km straight line substitute diameter surface three rivers tigated tributaries UNIVERSITY OF MICHIGAN values GQ vertical configuration