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<br /> ~.~!~?n1 <br />I '.' '... ~"",,' '-J 1 <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 />BIJOU AND KIOWA CREEK VALLEYS <br /> <br /> <br />Approximately 8 miles south of the South Platte River, the <br /> <br /> <br />al11uvial deposits of Bijou and Kiowa Creeks merge into a <br /> <br />common aquifer. The valley fill is 5 to 10 miles wide in the <br /> <br /> <br />B100u Creek valley; 1 to 3 miles wide in the Kiowa Creek valley. <br /> <br /> <br />Th~ckness of the alluvium in the Bijou Creek valley varies from <br /> <br /> <br />ldo to 240 feet. That in the Kiowa Creek valley exhibits an <br /> <br /> <br />a~erage depth of 85 feet. <br /> <br /> <br />BArGER CREEK VALLEY <br /> <br /> <br />Th~ area IS underlain by pierre shale, a formation not typically <br /> <br /> <br />us~d for ground water production because of small yields. Well <br /> <br /> <br />yi~lds in the Kiowa and Bijou Creek valley fill range from <br /> <br /> <br />400 to 1,600 gpm. Recharge occurs from precipitation and flooding <br /> <br />of! Bijou and Kiowa Creeks. <br /> <br />The valley fill of Badger Creek ranges in width from 0.5 mile <br />at; the Washington-Morgan County Line to 4 miles at the confluence <br />of: Badger Creek and the South Platte River. <br /> <br />BEfVER CREEK VALLEY <br /> <br />Be~ve~ Creek valley fill ranges In width from 3 to 5 miles. <br />In, the southerly end of the valley, alluvium reaches a depth of <br />55;feet. At the downstream confluence with the South Platte, <br />thickness is on the order of 120 feet. pierre shale underlies <br />the alluvium of Beaver Creek valley. <br />, <br />, <br /> <br />f' <br /> <br />2- <br /> <br />!' <br />", J. ,a <br /> <br />,':, ~_ _,c" -._k;":~', ;,,<_ <br /> <br />;._ 11,< ' <br />~ .,;:m..",1ic <br /> <br /> <br />2-13 <br />