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- occur within Desolation Canyon where the Wasatch formation forms the prominent cliffs. <br />In the Coal Creek reach, the canyon is formed within the Mesaverde Group. Schmidt and <br />Rubin (1995) reported on the reach scale geomorphic characteristics of Desolation and <br />Gray Canyons. <br />WORK CONDUCTED IN 1995 AND 1996 <br />The following work activities have been conducted: <br />1. Survey the topography and baythmetry along 22 cross-sections, located at <br />approximately 1-mi intervals in the four study reaches, and two other cross-sections located <br />elsewhere; <br />2. Resurvey along these cross-sections at 4 different times and different discharges <br />in order to determine the range of annual scour and fill and to estimate the stage-to- <br />discharge relation in each study reach; <br />3. Mapping of the surFicial geology in each study reach; <br />4. Mapping of the distribution of eddies and low-velocity zones at different <br />discharges; <br />5. Entry of these mapped data into a geographic information system, using <br />Arc/Info, and using geo-referenced locations; and, <br />6. Retrieval from archival sources of historical photos depicting the canyons as <br />early as 1917, and matching these photos. <br />METHODS <br />ChannE,-l Cross Sections <br />We established 22 channel cross-sections in the four separate study reaches and 2 <br />cross sections outside of the main study reaches, to characterize channel geometry, identify <br />bed material, and establish long-term channel monitoring sites. Five to six cross sections <br />were surveyed at about 1-mi intervals within each of the four study reaches. These cross <br />sections were established in 1995 at approximately bankfull discharge using a geodetic total <br />station and depth-recording echo sounder. Cross-section endpoints were monumented <br />4