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<br />. <br /> <br />. <br /> <br />THE FLOOD BELOW PUEBLO. <br /> <br />33 <br /> <br />Time of /foorl /lorc nt pn;,,'., mt-F'ormtnlll Creek. <br /> <br />. Point of observation. <br /> <br />Dl3tancc <br />above <br />mouth. <br /> <br />Approximate time or nOOll <br />flow. <br /> <br />\ <br />Butt............................................................ <br />.~:ro:;~:::::::::::::::::::::::::::::::::::::::::::::::::::::::: <br />~d~~~I~::::::::::::::::::::::::::::::::::::::::::::::::::::::: : <br />}Iouth......................................................... . <br /> <br />Jliks. <br />28 <br />23 <br />15 <br />11 <br />~ <br />n <br /> <br />11.1.5 p. m. June :l.1I <br />Between 11 and 12 p. In. <br />11.30 p. m. <br />About midnight. <br />After midnight. <br />3 a. m. June 4. <br /> <br />. <br /> <br />II Flood came very suddenJy. <br />Stnoe and di..oharoe of Fo,,"ta;1I Creek nt lIIolI/h. <br /> <br />Tim.. <br /> <br />Approxi. <br />matedis. <br />charge. <br /> <br />Stage. <br /> <br />.. <br /> <br />. . __ . Srrrtnd-lttt. <br />lune 3, ~tfdg:ghi::::::: :::: ::::::::::::::::::: "2:5 feet'dccp:400 irei'\~.i(i~::::::: :::::::::::: t,~ <br />June 4, 2.30 B. In.. ......... ................... n reet deep, .JOO (eet whIt... ................. 12,OCXJ <br /> <br />~:: E:::::::::::: ::::::::::::::: :::::: '~';:~:~i~;;~r~i:::::::::::: ::: ::::::::::::: ~t~ <br />Mfdntght.......... ................ .... -& tcct 1X!low ('rest............................ 18,000 <br />June 5, 5 a. m... ...... ... ..... ................ r,. feet belo\v crest............. ............... t!,OOO <br />5 p. m......................... ..... ... 7 feet below' crest...... ...................... 10,000 <br />June 6,3 p. m....... .... ...................... .. ......... ..... ......... ......... ............1 .1. 000 <br />, <br /> <br />The total dI~hnrge wa." ahollt 70,000 acre-fecl. <br />ST. CKARLES RIVER. <br /> <br />. St. Charles River drains the eastern slope of the southern half of <br />the Greenhorn Range and the foothill region lying betwe'en that <br />range and the Arkansas. After leaving the mountains the St. <br />Charles flows through a canyon for 10.miles, below which the valley <br />widens, and the river finally emerges upon the plain, across <br />which it flows in a northeasterly direction to its junction with the <br />Arkansas, 8 miles below Pueblo. Its chief tributaries are Spring <br />. Branch and Greenhorn Creek. The topography of its drainage basin <br />is very rough, as the stream traverses the steep slopes of the moun- <br />tains, the deeply eroded foothill region, and the rolling plains next <br />to the Arkansas. The drainage' area is 482 square miles. <br />The following table has been compiled from topographic maps: <br /> <br />Ele-vntioll.' and di..tanee.. a:tollO Sf. Cllar'les Ri'ver from SOlt1"Ce to mOlllh. <br /> <br /> EleTa- Dbtance. Descent between <br /> tion points. <br />Point. above I <br /> sea level. From Point to Total. Perroile. <br /> source. point. <br /> Fed. Mil... MiltS. Fed. Fttt. <br />SOUTce.............................................. . 9,000 u""6."5" ..,.uti.S' u'"2"750' .......... <br />Contour crOS$ing..... ..... ................. ... ....... 6,2.'50 420 <br />Do.............................................. 5,150 10.7 I '.2 '500 119 <br />D').............................................. 5,250 IS. 5 7.8 500 6' <br />Do.............................................. 5,000 24. 7 6.2 250 40 <br />Do................................................ 4,800 al.9 i 7.2 200 28 <br />Do... 4, iOO :!6.0 '.1 100 2< <br />Do...:::::::::::::::::::::::::::::::::::::::::.:: 4,6CO .,l~. 1 I '.7 100 21 <br />: <br />~ronth............................................ "'l ',560 .1. 9 1.2 41l :i3 <br /> ! <br />-. .-. - -_.- <br /> <br />S415S0-22--3 <br />