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<br />. <br /> <br />( <br /> <br />. <br /> <br />Animas the overflow reached First Street which wss not as <br />severe as the 1921 flood when it was 4 feet deep at that lo- <br />cation. Below the mouth of the Purgatoire River, the flow was <br />estimated at about 25,000 c.f .s. <br /> <br />. <br /> <br />20. FLOOD OF 1904. A storm occurrin~ during the period <br />September 27 to October 1 caused severe flooding on the Purga- <br />toire River at Trinidad and in the valley in both directions <br />from that city. The storm originated mostly on the Purgatoire <br />River watershed with heavy concentrations at and above Trinidad. <br />The flood was the largest of record in that vicinity. Tribu- <br />taries other than the Purgatoire River contributed to heavy flow <br />in the Arkansas River where the peak flow st Lamar was estimated <br />at 65,000 to 70,000 c.f.s. <br /> <br />I <br />,. <br /> <br />I. <br /> <br />21. FLOOD OF 1906. Heavy concentrations of storms in the <br />Big Sandy Creek area during the period October 17-19 extended to <br />the Purgatoire River and the Arkansas River between Las Animas <br />and Lamar. There was no flood at Pueblo, but below the mouth of <br />the Purgatoire River the peak flow was estimated at 80,000 <br />c.f.s. <br /> <br />. <br /> <br />(" <br /> <br />22. FLOOD OF 1921. On June 1 a cold front passed over <br />Colorado and by early morning on June 2 a high pressure area, <br />centering over northern Canada, extended entirely over the <br />state. By June 3, a weak, low-pressure area had formed over <br />southern Arizona and northwestern Mexico. Strong anticyclonic <br />circulation brought relatively moist, possible modified con- <br />tinental air into Colorado. Orographic action was pronounced <br />and heavy precipitation occurred along the fronts. Two areas of <br />intense rainfall were observed above Pueblo. One of these was <br />mostly north of the towns of Florence and Canon City. The other <br />fairly well distributed on both banks of the Arkansas River <br />between Portland and Pueblo. Precipitation in this latter <br />area is reported to have been as much as 11 inches in 6 hours <br />while in the other area it was reported to have been as much as <br />9 inches in 6 hours. The rainfall in the upper area was re- <br />ported to have occurred first so that runoff combined with that <br />below produced the largest flood of record at Pueblo. The main <br />center of the storm was on Dry Creek and there were heavy rains <br />at Pueblo and on tributary areas eaat of Pueblo. Areas in <br />Huerfano and Purgatoire Rivers and in Timpas, Adobe, and Horse <br />Creeks were flooded by runoff from heavy precipitation. Heavy <br />rains occurred on the main stem of the Arkansas River from La <br />Junta to Lamar. Four peaks were observed at Pueblo during this <br />flood. The first occurred about 2 a.m. on June 3. The .second, <br />and largest, occurred at midnight on June 3,and two smaller <br />peaks were observed on June 5. The peak discharge at 2 a.m. on <br />June 3 was about 28,000 c.Ls., and that at midnight waa 103,000 <br /> <br />I. <br /> <br />I <br />. <br /> <br />. <br /> <br />I. <br /> <br />7 <br /> <br />. <br />