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<br /> <br />35. Flood frequency.-Floods, L 0., discharges exceeding bank- <br />full stages, may be expected more frequently in particular re,aches <br />because of the varying channel capacitios. A curve of probable flood <br />occurrences was constructed for Purgatoire River at Trinidad by <br />standard methods, using the period of record from Jime 1922 through <br />June 1942. Rcliable and historical flood records indicate that five <br />floods exceeding a discharge of 30,000 cubic feet per second have <br />. occurred during a period of 76 years. An inspection of the probable <br />flood occurrence curve for Trinidad indicates that five or six floods <br />equaling or exceeding this magnitude may be expected per 100 years <br />(cbart No.6, appe,ndix B).' As a period of 21 years and 17 years <br />elapsed between the 1904,1925, and 1942 major floods, and five major <br />floods occurre,d which exceeded 30,000 cubic feet per second during 76 <br />, years of record, it was conclu(led that the probable flood occun'ence <br />curve. constructed from the period of record from June 1922 to June <br />1942, is represcntative of flood occurrences per 100 years. ' <br />36. Designjlood criteria.~The maximum flood of record at Trinidad <br />eccurrcd in September 1904 when a peak discharge of 45,000 cubic feet <br />per second and a volume of approximately 50,000acre,feet were <br />estimated.. Frequ~ncy investigations at Trinidad indicated that .a <br />flood of thiS magllltude would occur about, once III 100 years. It IS <br />considcred that the design of flood-control improvements should be <br />based on providing adequate protection against a flood of this magni- <br />tude if found economically feasible. Such a degree of protection <br />would avoid inducing a false sense of )lecurit,y which might be engen- <br />dered by improvements designed to provide flood protection for floods <br />of lesser magnitude. Plans investigated and recommended are dis, <br />cussed in paragraphs 60 to 78. <br />37. Maximum probable flood.-The maximum probable flood was <br />developed from consideration of the maximum probable rainfall occur- <br />ring when minimum loss rates prevailed in the drainage area under <br />consideration. A peak discharge of 127,000 CUbic feet per second and <br />run,off volume of 175,000 acrecfeet were computer! for these conditions. <br />The maximum probable flood hydrograph is shown on chart No.9, <br />appendix B.' The development of the maximum probable flood is <br />given in appendix B.' <br />38.' Extent and character of jlooded area-General.-Although there <br />are areas subject to ovorflow in other portions of the main valley <br />and on the tributaries, the most impertant are along the main stem <br />upstream from the head of the canyon section, near Alfalfa, to the <br />Sopris Dam site. The probable overflow area is indicated on maps <br />Nos. 2 to 7, inclusive,' appendix A. In this portion of the flood plain, <br />which includes that in Trinidad, there is a total of 5,000 acres of <br />which 370 acres are urban lands. Between Alfalfa and the mouth of <br />the river, there are some cultivated areas, but they are relatively <br />unimportant. Flood damages in this portion of the valley are not <br />extensive, and crop damages are limited largely to the vicinity of <br />Higbee and the agricultural Rrea below the mouth of the canyon. <br />Major floods cause some damage to the irrigation ditches, diversion <br />dams, and the bridges. There are no important overflow areRS in <br />Long Canyon. <br />39. Extent and character of jloodedarea-1'rinidad.-An area of <br />370 acres in Trinidad is in the overflow plain. This contains rail, <br /> <br />1 Not printed. <br />