Laserfiche WebLink
<br />w <br />~"-'" <br />o <br />CO <br /> <br />List of Figures (continued) <br /> <br />Figure Page <br /> <br />5-35 Accumulated salt versus accumulated sediment for channels <br />1-1 (a) and 2-1, (b) run 3 (after White, 1977)........... 134 <br /> <br />5-36 Average EC versus hillslope inclination for Hills10pe <br />Studies I and II (after Shen et aI, 1981)................ 135 <br /> <br />1 <br />I <br />I <br /> <br />5-37 Effect of flow velocity on dissolution rate of soluble <br />minerals from Mancos Shale (a) after SUnday, (1979) and <br />from channel material (b) (after Nezupati, Bowles and <br />Riley, 1981)............................................. 136 <br /> <br />5-38 <br /> <br />6-1 <br /> <br />6-2 <br /> <br />7-1 <br /> <br />7-2 <br /> <br />7-3 <br /> <br />Variation of average EC (denoting dissolution rate when <br />divided by the duration of the experiment) with average <br />velocity (after Sunday, 1979)............................ <br /> <br />il <br /> <br />137 <br /> <br />Relation between valley-floor slope and drainage area for <br />small drainage basins I Piceance Creek area, Colorado <br />(from Patton and SChumm, 1975)........................... <br /> <br />SChematic longitudinal profile of an active channel <br />showing identifiable features............................ <br /> <br />145 <br /> <br />I <br /> <br />146 <br /> <br />Relation of chemical dendation (D) to relief of small <br />watersheds (from Alexander, 1985)................,....... <br /> <br />Stages of erosional evolution of South African gullies <br />(from SChulllfTl, 1985)...................................... <br /> <br />l53 <br /> <br />154 <br /> <br />I <br /> <br />Hypothetical change of sediment production and active <br />channel (gully) drainage density with time (from Schumm, <br />1985). . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. . . . . . . . . . . <br /> <br />l56 <br /> <br />I <br /> <br />! <br /> <br />,I <br /> <br />vi <br />