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Last modified
1/26/2010 2:48:47 PM
Creation date
10/12/2006 3:05:01 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8141.100
Description
Fryingpan-Arkansas Project - Project Description
State
CO
Basin
Arkansas
Date
1/1/1969
Author
US DoI BoR
Title
Flood Control Fryingpan-Arkansas Project Eastern Slope Features
Water Supply Pro - Doc Type
Project Overview
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<br />, (< <br />4 11. \,i <br /> <br />i ! <br /> <br />27. FLOODS. - Historical records incl~de re'feren~e to many f~;oods <br />in the.Arkansas valley above John Martin Re~ervoi!. The earliest known <br />flood 1n the area occurred in 1826, long before p:ermanent settlement in <br />the valley. Other reported floods occurrediin 1~59, 1864, 1869, 1886, <br />and 1894. These floods were generally conf~ned t'o the reach from Pueblo <br />downstream to below the present site of JOhil, Martin Reservoir. <br /> <br />28. FLOOD OF JUNE 1921.- Weather Bur~au r~cords show that during <br />the period 2-4 June 1921, precipitation over the watershed between Canon <br />. City and Pueblo was from three to five inch~s for the 48 hours ending <br />the afternoon of 4 June. The streams that ~nter 'the Arkansas River' <br />between Canon City ana the mouth of Chico Creek, '16 miles below Pueblo, <br />were the principal contributors to the flood. T"e flood wave increased <br />rapidly as it progressed downstream. Floodflows .from many tributaries <br />contributed to flooding at Pueblo and caused the ;flood of record. The <br />peak discharge at Pueblo was 103,000 c.f.s.) whi~h increased to 200,000 <br />c.f.s. when it reached La Junta. Above La ~unta 'the effects of valley <br />storage on peak attrition was obscured by tribut~ry inflow. Belo~ La <br />Junta the tributary inflow was small 'and the valley storage effect more <br />marked, as evidenced by the decrease in peak discharge to 187,000' c.f.s. <br />at Las Animas and to 165,000 c.f.s. at Lamar. ' <br /> <br />29. FLOOD OF MAY 1935.- The flood of 30 May 1935 on Monument <br />Creek, the principal tributary to Fountain Creek. was the maximum known <br />but resulted in little damage at Pueblo where Fountain Creek flows into <br />the Arkansas River. The flood peak, which was considerably reduced by <br />the time it reached Pueblo, was estimated tp be 35,000 c.f.s. near the <br />mouth of Fountain Creek. This flood was prpduce4 by an excessive: rain- <br />fall of short duration over an area or-less! than :100 square'miles in <br />the Monument Creek watershed, following a period!of general precipitation. <br />There were reports of as much as seven and eight linches of rainfall in <br />24 hours at several locations in the storm area. ' This flood caused <br />severe property damage and the loss of four live~ in Colorado Springs <br />and vicinity. <br /> <br />.' <br /> <br />, <br />I i <br />30. FLOOD OF APRIL 1942. - The month' pf Aptil 1942 was one of the <br />wettest months in Colorado's history. The ~verage precipitation of <br />4.53 inches was the second largest of record for 'the State at that time. <br />This amount was exceeded only by the 5.96 ihches of precipitation during <br />April 1900. Heavy precipitation, much of i~ in the form of snow, oc- <br />curred during 16-20 April over the Purgatoire River watershed. Rainfall <br />during the period 22-25 April hastened the melting of heavy snow deposits <br />causing high flows on the Purgatoire River ,at Las Animas. Precipitation <br />over the Arkansas River watershed above Las! Animas produced a peak of <br />12,000 c.f.s. at Nepesta, 34,000 c.f.s. at !La Junta, and 23,600 c.f.s. <br />at Las Animas. Although there was major fl100ding at ,Trinidad, where <br />the peak flow on the Purgatoire reached 27,iooo c.f.s., the principal <br />damage in the Arkansas River valley was to ~ransportation and irriga- <br />tion systems. <br /> <br />10 <br /> <br />'II <br />1! <br />"< <br />:; <br /> <br />I', 'I <br />, <br /> <br />-"- <br /> <br />i :; <br /> <br />;' <br /> <br /> <br />, , <br />! ' <br /> <br />.' <br /> <br />-' <br /> <br />,) <br />.. I <br />I <br />I' <br />I <br /> <br />; <br /> <br />i I <br /> <br />." <br /> <br />. <br /> <br />, "'t~ <br /> <br />-~,".;~ <br />~ . i; <br /> <br />" ',":;:' <br /> <br />~ <br /> <br />'i <br /> <br />. <br />
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