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<br />8.3.2 Changes in channel-margin deposits. . . . . . . . . . . . . . . . . . . . . . 79 <br />9.0 Analysis of NAU Survey Data, 1990 to 2001 . . . . . . . . . . . . . . . . . . . . . 82 <br />9.1 Methods................................... 82 <br />9.2 Changes in Area and Volume in the Post-Dam Flood Zone. . . . . . . . . . . .. 82 <br />9.3 Changes in Area and Volume in the Fluctuating Flow Zone. . . . . . . . . . . .. 86 <br />9.4 Changes in Volume in the Deep Parts of Eddies, Below the Stage of227 m3/s . .. 89 <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 />10.1 Summary....................................... 91 <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. . . . . . . . . . . . . . . . . . . . . . . . . . 95 <br />Acknowledgments. . . . . . . . . . . . . . . . . . . . . . . . . . . . . 96 <br />11.0 Literature Cited. . . . . . . . . . . . . . . . . . . . . . . . . . 97 <br />Appendices. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 103 <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />IV Contents <br />