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<br />34 <br /> <br />Progress of <br /> <br />CONTRIBUTIONS TO HYDROLOGY, 1937 <br /> <br />flood create on the Arlkaree and Republican rivers <br />above Benkelman, Nebr., May 31, 1935 <br /> <br />distances are valley miles, which represent more 0100611 than river <br />m1.1e8 the dlstancee traveled. by the flood crost.). <br /> <br />Approximate Elapsed Hate ot <br />time of crest time Distance travel (miles <br />(Central time) (hours) (miles) per hour) <br /> <br />(Th. <br /> <br />Point on river <br /> <br />First crest, which coInoided wIth main flood on <br />t.he South Fork or the Republioan River <br /> <br />Arlkaree at <br />Haigler, Nebr. <br />Republican at <br />Parks, Nebr. <br />Republican above <br />Benkelman, Nebr. <br /> <br />4&30 a.m. <br /> <br />7 a.m. <br /> <br />'" 8.m. <br /> <br />Arlkaree at <br />Cope, Colo. 3115 a.m. <br />Arlkaree north <br />of Idalia, Colo. 7130 a.m. <br />Arlkaree at <br />Haigler, Nebr. 11;30 a.m. <br />Republican at <br />Parks, Nebr. 1:30 p.m. <br />Republican above <br />Benkelman, Nebr. 3130 p.m. <br /> <br />2.5 <br /> <br />2 <br /> <br />Second orest <br /> <br />0.0 <br /> <br />4.25 <br />4 <br />2 <br /> <br />2 <br /> <br />11 <br />,2 <br /> <br />o <br /> <br />31 <br />27 <br />11 <br />,2 <br /> <br />4.4 <br />6.0 <br /> <br />7.3 <br /> <br />6.8 <br />5.5 <br /> <br />6.0 <br /> <br />Crest <br />disoharge <br />( sec.-ft.) <br /> <br />20,000 <br /> <br />25,000 <br /> <br />54,000 <br />50,000 <br /> <br />Progress of flood crest on South Fork of Republican River and on Repub- <br />lican River between Benkelnmn, Nebr., and Junction City, Kans. <br /> <br />(Distances are valley milee.) <br /> <br />Point on river <br /> <br />Newton, Colo. <br />St. Francis, <br />Kans. <br />Benkelman, Nebr. <br />Yox <br />Trenton <br />Culbertson <br />McCook <br />Cambridge <br />Oxford <br />Bloomington <br />Franklin <br />Superior <br />Hardy <br />Scandia, Kans. <br />Concordia <br />Clay Center <br />Wakefield <br />Milford <br />Junction City <br />(water plant) <br /> <br />Approximate <br />time of crest <br />( Central time) <br /> <br />May 31, 3 8.m. <br /> <br />4 il..ill. <br />9 a.m. <br />9:45 a.m. <br />Noon, <br />1130 p.m. <br />3130 p.m. <br />8 p.m. <br />June 1, 1 a.m. <br />10130 a.m. <br />Noon <br />June 2, 1 a.m. <br />2130 a.m. <br />S a.m. <br />11130 a.m. <br />June 3, 2 a.m. <br />7 a.m. <br />10 a.m. <br /> <br />2 p.m. <br /> <br />~lapsed <br />time <br />(hours) <br />o <br /> <br />1 <br /> <br />5 <br />.75 <br />2.25 <br />1,5 <br />2 <br />4.6 <br />6 <br />9.5 <br />1.6 <br />13 <br />1.6 <br />3.5 <br />5.5 <br />14.5 <br />6 <br />3 <br />4 <br /> <br />Distance <br />(miles) <br />o <br /> <br />26 <br />8 <br />20 <br />10 <br />10 <br />26 <br />28 <br />36 <br />4 <br />49 <br />7 <br />16.7 <br />18.0 <br />37.0 <br />13.6 <br />6.8 <br /> <br />11.3 <br /> <br />Rate of' <br />travel (miles <br />Der hour) <br /> <br />* <br />6.0 <br />10.7 <br />8.9 <br />6.7 <br />5.6 <br />6.6 <br />5.6 <br />3.B <br />2.7 <br />3.B <br />4.7 <br />4.B <br />3.3 <br />2.6 <br />2.7 <br />2.3 <br /> <br />2.B <br /> <br />Crest <br />d18charge <br />( 8ec.~!'t.l <br /> <br />190,000 <br /> <br />245,000 <br />.. <br /> <br />260,000 <br /> <br />225,000 <br />215;000 <br />195,000 <br /> <br />+168,000 <br /> <br />Not comparable, as rainfall on intermediate areas increased the di.- <br /> <br />* <br />charge. <br />** The max1mum <br />anu i8 estimated as <br />t Above mouth <br /> <br />crest discharge occurred between <br />about 280LOOO second-teet. <br />of Smoky Hill River. <br /> <br />Cambridge &.nd Arapahoe, <br /> <br />- r------ <br /> <br />FLOOD ON REPUBLICAN AND KANSAS RIVERS, YAY AnD JUNE 1935 <br /> <br />35 <br /> <br />Progress of <br /> <br />flood crest on Kansas River between Junction City and <br />Kansae City, Kans., June 3-7, 1935 <br /> <br />(Distances are valley miles.) <br /> <br />Rate of <br />travel (miles <br />per hour) <br /> <br />]!:lapsed <br />t1m. <br />(hours) <br /> <br />Point on river <br /> <br />Approx1mate <br />time of crest <br />( Central time) <br /> <br />Crest <br />discharge <br />{ sec.~ft.l <br /> <br />Distance <br />(miles) <br /> <br />JW1ct1on City <br />(Below Smoky <br />Hill River) <br />Ogden <br />Manhattan <br />(Above Big <br />Blue R1 ver) <br />(Below Blg <br />Blue River) <br />Wamega <br />Topeka <br />Bonner Springs <br />Kansas City <br /> <br />June 3, 2 p.m. <br />9130 p.m. <br /> <br />7.5 <br /> <br />1.0 <br /> <br />17g ,000 <br />170,000 <br /> <br />7.5 <br /> <br />B.O <br /> <br />11.5 <br /> <br />1.4 <br /> <br />160,000 <br />190,000 <br />177,000 <br />154,000 <br />122.000 <br />120.000 <br /> <br />June 4, 6130 a.m. <br /> <br />do <br />June 4, 3:30 p.m. <br />June 5, 2 p.m. <br />June 6, 8110 p.m. <br />June 7, 5 a.m. <br /> <br />14.3 <br />37.5 <br />49.0 <br />17.0 <br /> <br />1.4 <br />1.7 <br />1.6 <br />1.9 <br /> <br />10.0 <br />22.5 <br />30.1 <br />B.B <br /> <br />Note.- The f'lood peaks at Bonner Springe and at Kansae City were flat <br />and of long duration. therefore it W8-S difficult to determine the exact timee <br />of the momentary maxima at those places. The determinatIon of the crest dis~ <br />charge at Kansas City ie only approx1mate. <br /> <br />Duration of fiood crest <br /> <br />North of Seibert. Colo., the Republican River rOS6 quickly to its peak <br />about midnight May 30-31 and remained there for ebout an hour, then r~c6ded <br />gradually. <br />Near Newton, Colo. (sec. 20, T. 5 S., R. 43 w.l, the river started to <br /> <br />r1se at 10 p.m. May 30 8nd reached a stage of 11 feet at :3 a.m. May 31. It <br />then fell 2 feet during the next 2 hours and was back In its banks at a stege <br />of :3 feet in the evening. The overflowed area had 8- width of 4,700 f'eet, and <br /> <br />the water wna about 8 feet deep. Only one crest was reported. <br /> <br />Below Ntlwton, 1..wo croHto dovulopod UtJCUUiJO of 1..1ll) bouvy l'ulrd'nll 1l0rLIL- <br /> <br />ea.!!t of thut point. Near the Kan:Jas-Nobrasku line south of llenkelman, Nebr., <br /> <br />a rancher measured the rise and fall of the river by moane of 8~inch concrete <br /> <br />blocks in the foundation of hie resiuence near the river. At 11 p.m., al- <br />though there was a heavy rain, no sign of a flood appeared. but by 3 a.m. the <br /> <br />river hud risen 7 feet, and at 9 a.m. it reached ite crest of 10 feet. It <br />then fell 2 feet during the next hour and rose to a socond creat of 9.5 feet <br /> <br />at 1:15 p.m. Thie second cretlt, like the fir3t, was of short duration, and <br /> <br />the r1ver fell to a stage or 7.5 :foet by :5 p.m. A third rise 01' hal:f Ii root <br /> <br />occurred within the next hour, after which the water receded very 1310w1y to <br /> <br />the bank-full stage of 6 feet. The width of' the overfiflwed area WliS threo~ <br /> <br />quartera of a mile. <br />At. Max, Nebr., t.he river reached its crest of 11.8 teet about 9:45 <br /> <br />a.m. and then fell to Ii stage of 8.8 feet by 11 n.m. It renched a second <br />