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<br />, <br /> <br />I <br />I <br /> <br />16 THE ARKANSAS RIVER..ELOOD OF JUNE' H, 1921. <br /> <br />The statements of local residents and the measured maximum dis- <br />charges of the tributary streams indicate two principal areas of <br />intense rainfall. (See Pl. I.) The larger area, which is roughly ellip- <br />tical, extends from the northern boundary of Pueblo County to the <br />top of the 'Wet Mountains near Beulah, a distance of 30 miles, and <br />from a point a short distance above the mouth of Rush Creek nearly <br />to Pueblo, a distance of 15 milt's. The smaller area covers the south <br />slope of the Pikes Peak uplift, which forms the northern part of <br />tIle m?untain valley, nnd e:'i:tends from a point above Skaguay reser- <br />voir to a point 3 or 4 miles south of the river, a distance of 25 miles, <br />and from Oil Creek to Beaver Creek, a distance of 11 miles. The two <br />areas coyer ~5'p square miles. . <br /> <br />. <br /> <br />EFFECT OF RESERVOIRS ON THE FLOOD. <br /> <br />Considerahlt! misinformation relat,ive to the effect of reser.oirs <br />upon the flood was dis.<;elllinated hy thl) hrt)n',n'1I1 iuul lcdlllical press <br />at the time of its O<:f'UITI'JU:t'. There 111'1) three reservoirs of con- <br />siderable size within the areas 0 r intense rainfltll, antlnone of these <br />contributed to the main flood of .June 3. The Schaeffer reservoir, <br />on Beaver Creek, failed 011 June 5,causing the flood of that date, <br />which was very severe in the yalley immedi!1tely below the mouth of , <br />Beaver Creek but flattened Gut farther downstream. The other two <br />reservoirs, the Skaguay reservoir, on Beaver Creek, and the Teller <br />reservoir, on Turkey Creek, safely withstood the flood. At the time <br />of the main flood the three reservoirs helped in a slight degree to <br />reduce its magnitude by holding back a portion of the run-off above <br />them. <br />The Schaeffer reservoir, which had a capacity of 3,190 acre-feet, <br />was formed by an earth dam across Beaver Creek in sec. 9, T. 18 S" <br />R 68 W. The dam had a maximum height of 100 feet above the <br />bottom of the outIet and a length on the: crest of 1,100 feet. ; Its <br />average height was about 90 feet for the middle 500 feet of'its <br />length. The width on the crest was ,15 feet, the outside slope 2 to 1, <br />",and the inside slope 3 to 1. .A freeboard of 10 feet was provided. <br />..A concrete cut-off wall ,",,'as provided in the middle portion of the <br />dam, and a timber cut-off wall for the remainder, The inlet was a <br />concrete tunnel'{ feet wide and 5 feet high, t'onstructedon bedrock. <br />The dam was built to a height of 20 to 30 feet by the hydraulie- <br />fill method when it was ohscrn:d tllat the 1I1aterial deposited in the <br />center of the dam retained water aml dill not cOllsolidate, being more <br />nearly liquid than solid. The liquid material ,\-as replaceu by dry <br />earth,' and the dam was finisher1 by depositing the earth by wagons, <br />sprinkling, and rolling in thin layers. The inner slope was rip- <br />rapped to the top. A spillway 100 feet wide was providell beyond <br /> <br />. <br /> <br />. <br />