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<br />I <br />I <br /> <br />I <br />I <br /> <br />;, <br /> <br />-- -.-- <br />THE FLOOD AT PUEBLO; <br /> <br />C) .j <br />~,) <br /> <br />THE FLOOD BETWEEN CANON CITY AND PUEBLO. <br /> <br />From Canon Ci~y to Florence, a distanell of H miles oy river, the <br />valley is coIIlparatlvely n,arrow and was little damaged by the flood. <br />The maximum discharge increased from 3,740 second-feet at CanOl) <br />City to 9:000 second-feet at Florence.s The tributary streams in this <br />section-Oil, Chandler, Sixmile, Oak, and Coal creeks-lie partly <br />within the upper of the two areas of intense rainfall but did not have <br />as high unit discharges as the tributaries nearer Pueblo. (See table <br />of maximum discharge, pp. 21-22.) <br />Between Florence and the mouth of Beaver Creek, a distance of <br />10 miles, the'discharge must have ,increased considerably, as the <br />principal tributaries, Eip;htmile, Brush Hollow, and Hardscrabble <br />creeks, had their flood crests between 7.30 and 8.30 p. m. on' ,Tune :3, <br />about the time. the river was highest at Florence. At Portlancl, 5 <br />miles below Florence, the highest water occurred at 11 p. m., when <br />the water was 4 feet (leep in the Dem'er &: Rio Grande Rll.ilroa(l <br />station.. The water started to fall here at 11.30 p. m. and in all hour <br />had fallen 3f feet. <br />From Beaver Creek to Turkey Creek, a distance' of 11, miles: the <br />maximum stag-e during- the evenin:r of ,Tune Jl could not have in- <br />creased very greatly, as the tributary streams, Rush and Red creeks <br />and Ritchie and Fred Rohr gulches, had their flood crests about 5 <br />p. m., several hours before the passage of the main flood crest in the <br />river. In this stretch the greatest damage was caused not by the <br />flood of June 3 but by that of June 5 due to the failure of the <br />Schaeffer reservoir on Beaver Creek (1'.17). (See PI. V, B.) <br />Between Turkey Creek and Pueblo the discharge of the river in- <br />creased very rapidly, as this was the section which received the maxi- <br />mum run-off from the areas of intense rainfaH. <br /> <br />THE FLOOD AT PUEBLO. <br /> <br />GENlolRAL' FEATURES. <br /> <br />'Pueblo, ,the second cityin size in the State, is on Arkansas River <br />a. few miles east of the foothill region and just above the mouth of <br />Fountain Creek. The 1920 census gave its population as 42,908. It <br />is nn important railroad center, being on the lines or the Atchison, <br />Topeka &; Santa Fe, Denver & Rio Grande vVestern, Missouri <br />Pacific, and Coloraclo 8:; Southern railways. It is also an important <br />m:\llllfacturing center, the steel mills: smelters, r'ailroacl car shops, <br /> <br />. F:nl:lnc~rs of the Denycr '" RIo Grande Railroad Co. measured a cross section of the <br />