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<br />CCC;" <br />;':"i" -,' <br />-':.". <br />"'-'~'- <br /> <br />.~...'.' <br />;:(~ <br /> <br />lower the salinity of the Colorado River by approximately 16 milligrams <br />per liter (mg/l) at Imperial Dam near Yuma, Arizona. <br /> <br />INTRODUCTION TO THE PROBLEM <br /> <br />Paradox Valley <br />Trending northwest-southeast, Paradox Valley is 3 to 5 miles wide and <br />about 24 miles long, and is crossed near its midpoint by the Dolores <br />River. The surrounding wa11s of sandstone and shale layers <br />are quite steep and rugged, while the floor itself is relatively flat and <br />featureless. With the exception of about 3,600 acres of irrigated crop- <br />land in the northwestern half, the area is generally undeveloped. The <br />major source of income is livestock, although some malting barley is grown <br />as a cash crop. The climate of the valley is generally arid; typically <br />hot and dry during the summer and cold and dry during the winter. <br /> <br />.Geophysicat. studies including deep. drilling by oil companies haveestab- <br />Ii shed the presence of a series of five major salt anticlines in south- <br />western Colorado and southeastern Utah. As shown in Figure I, the anti- <br />clinal region is about 100 miles long along its northwest-southeast axis <br />and is marked by the extrusive mass of the La Sal Mountains prominently <br />perched over its center. Paradox Valley, lying along the axis of one of <br />the largest al,ticlines, has been formed by the erosion of faulted and up- <br />lifted sandstone and shale formations, exposing a residual gypsum cap which <br />covers about 14,000 feet of pure salt and salt-rich shale. <br /> <br />Paradox Valley has been identified as a major natural contributor of <br />salinity in the upper basin. The Dolores River, in crossing the valley, <br />picks up an'estimated 200,000 tons of salt each year and carries this <br />load to its confluence with the Colorado River. <br /> <br />Geology <br /> <br />Figures 2 and 3 illustrate the development of the valley. Briefly stated, <br /> <br /> <br />the emergence of mountainous uplifts on each side of the area has placed <br /> <br /> <br />intense lateral pressures on the intervening sedimentary formations, <br /> <br /> <br />resulting in faulting and fracturing along weak zones. Under these pressures <br /> <br />3 <br /> <br />oor584 <br />