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<br />-~ <br />, <br />~ <br />, <br />, <br />i <br /> <br />\ , <br />1'..'.0--. <br />''-~' - . <br />\ ~',- <br />Ik. <br />'L~'-;' <br />~l.l. ,<,: <br /> <br />'. : <br /> <br />.'.f <br /> <br />~. . <br /> <br />" <br /> <br />J <br />f <br />1: <br />L. <br /> <br />i <br /> <br />THE FLOOD AT PUEBLO. <br /> <br />27 <br /> <br />,Tune 3, and because the area inundated was so wide it was impossibk <br />to make discharge measurements during the peak flow. A Her the <br />flood the United States Geological Survey determined the maximum <br />discharge as 103,000 second-feet. (See p. 20.) <br />An idea of the unprecedented discharge of the river during the <br />flood is given by the following table showing the available records or <br />maximum discharge: <br /> <br />Annual ma3Jimum discharge of A,rlcutr.sG.9 River at Pueblo for certain vear.'? <br /> <br />Dis- II Year. Date. I Dis- <br />charge. charge. <br />Sream!- Secf}nd~ <br />feet. feet, <br />4,530 1907.........,:,.... July 28. m......... 4,G-l <br />7660 1908. 0....,........0 Juno 1.'}-16........ 1,9? <br />0'520 1909... ............0 Aug. UL.......... 5, <br />39:100 19100.... ,....... ... Julle1............ S, <br />5,000 1911... '..0.0.... ,., JulyO............, 7,rx <br />3,440.. 1912. 0 ,.....0......0 June9.... ""'." 10,lX <br />3,750 1913:.. .............. July2.'L........... 7,80< <br />5,3&! Itl14. ............... Allg.3............ 7, <br />4,890 1915.. .............. 1une24........... 17,OC <br />6980 19160.. ............. June 17.'.. ........ 8, <br />10:700 1917. ..........,.... June 13........... 6, <br />8,320 1918,'.0.,..........0 lune2:L........__ 9, <br />6,100 1919., .............0 M.y30.....0...... 5 <br /> , <br />3,310 1920......,......,.. June 10...... ..... 4,& <br />6,460 1921., .............. Juno3.... ... ._... l():\ <br />4,880 <br /> <br />Year. <br /> <br />Date. <br /> <br />1885... ............. June 5. _.... ...... <br />1886..........,..... M.y29.o......,... <br />1887 ................ July 18...0........ <br />1894.....0...0....,. M.y 31.....,...... <br />1895.. ............. 'I' July 31............ <br />1896..........,..... Aug,180.......... <br />1897. _. ............. lune 2.... .... .._. <br />1898...........0.... July 13...,......., <br />1899... ... ........_. JWle 20.... ....... <br />1900...0.....0. ..... June 2... 0 ...,.... <br />1901......0......... May 21............ <br />1900... ............. Aug. 5... ,.,......, <br />1903.. _ ..._......... June 9. ... ......... <br />1004... ............. JW1C 15.... ....... <br />100.')... ...... ....... June 10.... ....... <br />1906.. 0 ............. June H... ........ <br /> <br />0,- <br />lO, <br />8(J(), <br />000 <br />~. <br />~ <br />) <br />500 <br />~ <br />900 <br />800 <br />600 <br />230 <br />~ <br />000 <br /> <br />. , <br /> <br />NOTE.-For 1901 and from 1909 t.o 1920 the discharge is that tor the ma:timum stage recorded. For <br />the other years the maximum discharge is that'for the 24-h(lur period. <br /> <br />- <br />TOTAL DISCHARGI,. <br /> <br />, 'the recording, gage at Pueblo was destroyed by the flood, and no <br />: con~inuous record of river height exists. From the testimony of local <br />i observers and from high-wllter marks it has been possible to ,con- <br />struct a fairly complete and accurate hydrograph of the Arkansas at <br />'Pueblo from June 2 to I),(fig. 1). The most complete record of the <br />river during the time of the principal rise' was that obtained hy MI'. <br />B. Milton Stearns, assistant chief train dispatcher of the Denver & <br />Rio Grande Railroad. As the water rose in the Union Depot the <br />distance to the water surface from a flxed point was measured with 'L <br />level rod and the time noted. This was done at frequent intervals <br />from 9 p. m. on the 3d to '"{ a. m. on the 4th, the period during which <br />the river was above the floor of the Union Depot. The reference <br />points used were latercomiected to the city datum by level, and -the <br />maximum stage was found to be at 4,t>84.75 fEEt above the sea. Tiie <br />maximum stage at' th:e:ri~e~ g&gtf x~: (fie Main Street bridge ~~,s <br />determined after 'thli' flood, from a well-defined water. mark on -t~e <br />outside of the new'dity'hh1J,150 feet distant. This mark was found <br />to be 24.66 feet above the zero 'of the gage, or 4,681.70 feet aboye the <br />sea, 3.05 feet lower thim the maximum observed at the Unipn Depot. <br />