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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />001104 <br /> <br />WHITE RIVER GEOTECHNICAL STUDY <br />FINAL REPORT <br />EXECUTIVE SUMMARY <br /> <br />The 1983 session of the Colorado General Assembly passed House Bill 1102, <br />authorizing the Colorado Water Conservation Board (CWC8) to conduct a <br />geotechnical study of dam sites in the White River Basin. Specifically, the <br />bill called for studying sites located at Powell Park, Lake Avery and two <br />si tes between the confl uence of the North Fork and South Fork of the Whi te <br />Ri ver and the Hi ghl and Ditch Headgate. In May of 1985, the CWCB contracted <br />with Morrison-Knudsen Engineers, Inc. (MKE) to perform the study. <br /> <br />The objective of the White River Geotechnical Study was to carry out surficial <br />and sub-surface geotechnical investigations of the designated dam sites, and <br />to locate and evaluate potential sources of construction material. The level <br />of topographic data on the reservoir areas was to be upgraded. In addition, <br />appraisal-level designs and cost estimates of various alternative dam <br />confi gurati ons were to be made, based on the fi ndi ngs of the geotechnical <br />investigation, as well as technical and economic comparisons of the sites. <br /> <br />The study was initiated by reviewing available reference material from <br />previously completed geological and water development studies carried out in <br />the White River Basin. A network of targets for air photogrammetry were set <br />and tied in to existing survey control. Aerial photographs were taken of the <br />potential reservoir areas and topographic maps at a scale of one inch to 500 <br />feet, with 10-foot contours were prepared. Aerial photography was also flown <br />for each dam site and topographi c maps at a scal e of one inch to 100 feet, <br />with 5-foot contours were prepared. <br /> <br />Field work started with general surficial geologic mapping of the study area. <br />The primary objective was to define the principal structural features and <br />lithologic units in the region. In addition, reservoir permeability and slope <br />stability of the potential reservoirs were evaluated. Borrow areas for <br />potential construction materials were also located during the surficial <br />mapping program. <br />