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<br />JV <br /> <br />CONTENTS <br /> <br />Major lIood&-CoDtlnUed. <br />Ark_ RlV...-cODtlnUed. <br />lIuerfaoo Rlver..__...._......._______.___________________ <br />ApbUuopaRlver._.____._____.__.__...._.._..___________.._ <br />PurgataaeRlver_________________.________.____._.________ <br />Wolf Creek and Granada Creek_.______________________.__.. <br />~Bu~te C>.ek._____..______.______________.__.____.___. <br />Wildllorse ~ek_____________.____.__________._____..____ <br />Minor tributaries of Arkansas Riveru_______________uu____ <br />lUa Grande___________________________________________________ <br />Sou~hFork RIo Grande__.....______________.______________ <br />Al&D008a~ek.______.__.......__._..________._...._._.___ <br />Conejos FUver____________________________________________ <br />Colorado River ____ _ _ _ __ ____ ___ _ __ __ __ __ _ _ _ _ _ _ _ _ _ _ _ ___ _ _ _ _ _ _ ___ <br />Gunn~on River___________________________________________ <br />lJncotnpa~ River___________________________________ <br />])olores FUver_____________________________________________ <br />W..~ Creek..___......._..__.___.____..._._.__________ <br />San Miguel River~ _ _ __________________________________ <br />SanJuan FUver___________________________________________ <br />Animas Fliver_________________________________________ <br />La Pl&ta River________________________________________ <br />Summary of maximum 69Qd discharges______________________________ <br />Changes in channel capacity and development of flood-protection measures <br />Index____________________________________________________________ <br /> <br />ILLUSTRATIONS <br /> <br />PLA.T8 1. City of Denver during the flood of May 19-20, 1864_ _________ <br />2. Damage to Denver &; Rio Grande Railroad caused by flood of <br />June 1921: A, Bridge w..~ of Pueblo; B, Railroad yards in <br />Puehlo..............._._........._._....._______...... <br />3. Damage to tracks of Denver &; Rio Grande Railroad caused by <br />flood of October 1911 on San Juan River near PagosaJunction_ <br />l'IotJU 1. Map of Colorado showing principal river systems and cities <br />mentioned in the text_______________n_________________ <br />2. Typical stage hydrographs of cloudburst floods_ _ _ _ _ _ _ _ _ _ _ _ __ <br />3. Chart showing maximum flood discharge. in eecond.feet per <br />square mile, for various places given in the summary table__ <br /> <br />Pqo <br />98 <br />99 <br />100 <br />111 <br />112 <br />112 <br />113 <br />114 <br />120 <br />121 <br />122 <br />123 <br />128 <br />123 <br />129 <br />130 <br />131 <br />132 <br />138 <br />139 <br />140 <br />148 <br />149 <br /> <br />FLOODS IN COLORADO <br /> <br />By ROBIllRT FOLLANSBIllIll AND LEON R. SA WYIllR <br /> <br />ABS'l'R.LCT <br /> <br />The firo~ records of floods in Colorado aDtedated ~he ..~tlemen~ of ~he , <br />by about 30 years. These were records of floods on the Arkansas and Repu <br />Rivers in 1826. Other floods noted by traders, hunters and emigrants, <br />of whom were on their way to the Far West, ocourred in 1844 on the ArH <br />River, and by inference on the South Platte River. Other early floods were <br />on the Purgatoire, the Lower Arkansas, and the San Juan Rivers about <br />The most serious flood since settlement began was that on the Arkansas <br />during June 1921, which caused the 1088 of about 100 lives and an e8th <br />property 1088 of $19,000,000. Many floods of lesser magnitude have Qce <br />and some of these have caused loBS of life and very considerable property da <br />Topography is the chief factor in determining the location of storms a1 <br />suIting floods. These occur most frequently on the eastern slope of the <br />Range. In the mountains farther west precipitation is insufficient to ca.use <br />except during periods of melting snow, in June. In the southwestern pa.rt <br />State, where precipitation during periods of melting snow is insufficient to <br />floods, the severest floods yet experienced resulted from heavy rains in SeptA <br />1909 aDd Oc~ober 1911, <br />In the eastern foothills region, usua.lly below an altitude of about 7,50 <br />and extending for a distance of about 50 miles east of the mountains, is a <br />8ubject to rainfalls of great intensity known as cloudbursts. . These cloudl <br />are of short duration and are confined to very small areas. At times the intA <br />is so great as to make breathing difficult for those exposed to a storm. The <br />of intenae rainfall are so small that Weather Bureau precipitation statioIlB <br />not been located in them. Local residents, being cloudburst conscious, freql <br />measure the rainfall in receptacles in their yards, and such records constitu <br />only source of information regarding the intensity. <br />A flood resulting from a eloudburst rises so quickly that it is usually des( <br />as a llwall of water." It has a peak duration of only a few minutes, follow <br />a rapid subsidence. Nearly 90 cloudburst floods in Colorado are deseril: <br />varying detail in this report. The earliest recorded cloudburst-called a1 <br />time a waterspout---occurred in Golden Gate Gulch. July 14, 1872. The Il~ <br />water" was described as a "perpendicular breast of 10 or 12 feet." A cloud <br />fiood on Kiowa Creek in May 1878 caused the 1088 of a standard-gage locom <br />and although search was made by means of long metallic rods, the loeomotiv <br />never recovered, as bedrock was about 50 feet below the creek bed. <br />All available information relative to floods in Colorado, beginning wit <br />flood of 1826 on the Arkansas River, is presented in this report, although for <br />of the earlier floods estimates of discharge are lacking. <br />Floods throughou~ a 1&rge part of ~he State have oceurred in 1844, JUDe <br />June 1884, May 1894, and June 1921. The highest floods of record were (l <br /> <br />I <br /> <br />P"". <br />84 <br /> <br />85 <br /> <br />140 <br /> <br />6 <br />8 <br /> <br />141 <br />