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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 />The MWE report identified a number of recommendations that should be pursued by the <br />District to further assess the status of the District's ground-water resources. At the <br />District's annual meeting on January 10, 2000, the District membership voted to accept <br />the recommendations in the report and to pursue additional studies of the District's <br />ground-water resources. MWE was subsequently contracted by the District to assess <br />the hydrogeology and water use in the District. This report addresses the finding of this <br />second investigation. <br /> <br />2.3 PREVIOUS INVESTIGATIONS <br />The U. S. Geological Survey (USGS) initially investigated the geology and ground-water <br />resources of Baca County in 1954 (McLaughlin). This study was followed in 1967 by the <br />above-referenced ground-water resources investigation by Beck and Associates. The <br />Colorado Division of Water Resources monitored ground-water levels in the Basin <br />beginning in 1987 and has published annual monitoring data (Roberts and others, 1990 <br />to 2000). The USGS published a report in 1999 documenting the water-level changes <br />from 1980 to 1997 and saturated thickness from 1996 to 1997 in the High Plains aquifer <br />(McGuire and Fischer). The Kansas Geological Survey has conducted a number of <br />ground-water use and water-level studies in southwest Kansas pertaining to the Dakota <br />aquifer (Macfarlane, et aI., 1993, 1995, and 1999). Each of these studies were reviewed <br />and relied upon for the Phase-1 investigation and report. <br /> <br />2.4 METHODS OF INVESTIGATION <br />In addition to a review of the published reports described above, selected well logs and <br />construction records kept in the official files at the State Engineer's Office and published <br />by the USGS (McLaughlin, 1954) were evaluated. These records were used to define <br />the hydrogeologic character of the aquifer system in the District and to create geologic <br />cross-sections and maps that are presented and described in this report. A brief field <br />review led by Max Smith, District board member, and accompanied by MWE team <br />members was conducted on July 10-11, 2000. Landsat satellite images from 1989 and <br />1999 were obtained to visually compare the change in land use and irrigation methods in <br />the District over this ten-year period. <br /> <br />11-3 <br />