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2) The importance of the data set to the integration of other studies or analyses. <br />3) The compatibility accuracy of the data set with the level of accuracy required within the <br />GCES/GIS. <br />4) The amount of editing necessary to bring the data set into a useful state. <br />The remaining studies will be integrated into the data base on an as-needed and availability <br />basis. <br />Of the 14 data sets used in the site No. 5 pilot, 7 data sets were used to illustrate the analytical <br />capabilities of the GCES/GIS and its applicability for protocol development. <br />A. Aquatics <br />1. Bathymetric and thermal mapping at the confluence of the Colorado and Little Colorado <br />Rivers, cross-referenced to indicate relationships and trends. <br />2. Data collected primarily to address questions regarding the endangered Humpback chub <br />(Gila cypha), including: <br />a. Net set locations with catch data from individual research trips. <br />b. Velocity contour maps at high and low flow, defining habitats in the current. <br />c. Shoreline habitat maps. <br />d. Radio telemetry information. <br />e. Minnow trap locations. <br />f. The thermal boundary at the confluence of the Colorado and Little Colorado Rivers <br />measured and delineated under different flow levels to identify optimum thermal <br />habitat for the Humpback Chub. This information will be combined with <br />bathymetry, radio-telemetry, and net set data to better identify habitat availability <br />and use. <br />g. River channel boundary at 5000, 15000, and 30000 ft3/s. <br />B. Terrestrial <br />1. Vegetation polygon data analyzed from aerial photography from 1963, 1984, 1990, and <br />1992 to identify trends in post-dam vegetation growth. <br />C. Sediment <br />1. Detailed sandbar surveys correlated with daily photographs of the subject sites to track <br />sediment aggradation and degradation at sites throughout the canyon. <br />2. A data set which monitors sediment movement throughout the canyon. Collection <br />methods included total station topographic surveys, bathymetric surveys, and <br />rectification of photographs taken daily during the time of lowest flow. These methods <br />were combined for a comprehensive look at sedimentation patterns. <br />11