Laserfiche WebLink
<br />9.0 <br /> <br />79 <br />82 <br />82 <br />82 <br />86 <br />89 <br /> <br /> <br />.002334 <br /> <br />8.3.2 Changes in channel-margin deposits. . . . . . . . . . . . . . . . . . . . . . <br />Analysis of NAU Survey Data, 1990 to 2001 . . . . . . . . . . . . . . . . . . . . . <br />9.1 Methods................................... <br />9.2 Changes in Area and Volume in the Post-Dam Flood Zone. . . . . . . . . . . . . <br />9.3 Changes in Area and Volume in the Fluctuating Flow Zone. . . . . . . . . . . . . <br />9.4 Changes in Volume in the Deep Parts of Eddies, Below the Stage of227 m3/s . . . <br />9.5 Long-term Changes Determined from Integration ofNAU Data with Aerial <br />Photograph Analysis. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 90 <br />10.0 An Integrated History of Fine.Sediment in Glen, Marble, and Upper Grand Canyons. . . . .. 91 <br /> <br />10.1 Summary......................................... 91 <br /> <br />10.2 Styles of Change in Eddies . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 94 <br />10.3 Style of Channel Change . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 95 <br />10.4 River Processes that Caused Channel Change and Constraints on Rehabilitation <br />Towards Pre-dam Conditions. . . . . . . . . . . . . . . . . . . . . . . . . . . <br />Acknowledgments. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . <br />11.0 Literature Cited. . . . . . . . . . . . . . . . . . . . . . . . . . . <br />Appendices. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . <br /> <br />95 <br />96 <br />97 <br />. .103 <br /> <br />IV Contents <br />