Laserfiche WebLink
<br />24 THE ARKANSAS RIVER FLOOD OF JUNE-8-5 1921. <br /> <br />, -- <br /> <br />foundries, and other manufacturing plants employing about 18,000 <br />men. The city lies mainly on the flood plnin of the river but extends <br />onto' the bluffs on either side. Originally the river pursued a wind- <br />ing course through the city, but its channel was straightened and <br />levees were built to furnish protection against a flood of 40,000 <br />second-feet, slightly greater than the maximum discharge of the flood <br />of 1894. ' <br />The heavy rains on .Tune 2 and 3 in the region west of Pueblo <br />caused several successive rises in the river. The highest rise and <br />the one that caused the great damage was the second, which oc'curred <br />on the night of June, 3. Dry Creek, which drains an area of 86 <br />square miles just west of Pueblo on the north side of the Arkansas, <br />!was subject to its severest flood the night of .Tune 2. This flood <br />baused the river at Pueblo to rise by 2 a. m. June 3 to a stage <br />'of 13.7 feet on the State gage just below the Main Street bridge. <br />This tise subsided in a few hours, and as the river channel could <br />safely carry a flood of that stage, little damage was done. The in- <br />tense rains that began on the afternoon of the 3d caused the river <br />to rise rapidly at 5 p. m., and by 8.45 p. m. the levees were overtopped <br />at a stage of 18.1 feet. The river continued to rise until at mid- <br />night the maximum stage of 24.66 feet was reached. This stage was <br />maintained for only a few minutes, and then the river fell almost <br />as quickly as it rose, until about 4 a. m. June 4 it had receded to <br />the top of the levee (18.1 feet). By 2.30 p. m. the river had fallen <br />to a stage of 9.5 feet and by midnight to 9.1 feet. About the time <br />the levees were overtopped they broke nt several plnces near the <br />west end of the city, am! large quantitics of water flowed directly <br />through the hellrt of the business sp,{ion. A third rise reached n <br />stage of 11.1 feet at ,~ a. ID. JUlle 5, but the river quickly subsi.lcll <br />again and relllllinetl at. a stage of V.l fcrt nnlil ~.l!i p. m., when a <br />fourth ,flood, causell by the breaking of the Schaeffer dam on <br />,Beaver Creek, reached the city. The river reached a stage of 13 <br />feet from 3 to 4 p. m. and then fell to 9.1 feet at 7 p. m. By this <br />time the flood run-oft from the area of heavy rains had passed, and <br />the river continued to recede gradually, except for a temporary rise <br />to S feet at 5.30 p.' m. June 6. <br />When the levees were overtopped an immense volume of water <br />flowed across the old flood plain and through the heart of the busi-, <br />ness section, which lies on both sides of the river. The area inun- <br />dated covered 3 square miles and extended from Sixth and Main <br />streets north of the river to the bluffs south of the Denver & Rio <br />Grande Railroad yards on the south side of the river. <br />~. . 11 ~_,_ _ .~ l-.ln ~h(\",,, t],p ],pi/J'ht of the high-water mark above <br />