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<br />I <br /> <br />Additional information on the Flood <br />available from local insurance agents or <br /> <br />Insurance <br />brokers and <br /> <br />Program <br />the: <br /> <br />i, <br /> <br />Continental Divide near Leadville, Colorado. Between Leadville <br />and Canon City it is a typical mountain scream with fairly steep <br />slopes descending more than 6,000 feet in elevation in 1\ distance <br />of about 130 miles. <br /> <br />Federal Emergency Management Agency <br />Division of Insurance and Mitigation <br />Building 710 <br />Denver Federal Center <br />Denver, Colo. 80225 <br />Telephone234-6582 <br />II. RELATED FLOOD STUDIES <br />A Special Flood Ha'l:ard Information report entitled "Arkansas <br />River, Anderson and King Arroyos, La Junta, Otero County, <br />Colorado" was published by the Corps of Engineers in August. <br />1977. This flood hazard study presented 1.nforlllation on the flood <br />hazat'da on the At'kansas Rivet' and ita tr1.butat'1.ea in the vie1.n1.ty <br />of La Junta, Colorado (Refet'ence 2). <br />The pt'eaent study extends ft'om the upstream limit of the Corps of <br />Engineers study on the Arkansas River for a distanee of <br />approximately 15.5 mile a to the v1.e1.nity of Roeky Ford. <br />Stream stationing in the present study on the Arkansas River was <br />continued from the upatream limit of the Corps of Engineers <br />study. Dischsrges and water surface elevation at the common <br />boundary of the two studies are identical. <br />The Corps of Engineers published in December, 1977, a report <br />entitled "La Junta Local Protection Project, Ls Junta, <br />Colorado" (Referenee 3). This study includes hydrologic analyses <br />for the La Junta area and agreea with the previously published <br />Special Flood Hazard Information Study. <br />The United Geological Survey Water Supply Paper 487 was published <br />in 1922 and givea information concerning the Arkansas River <br />Flood of June 3-5, 1921 (Reference 4). In 1966, a flood report <br />for the Arkanaas River Basin wall prepsred by the U. S. Army COrps <br />of Engineers (Referenc.. 5). This study deals with the Arkansaa <br />River Flood of 1965, and its effects on Colorado, Kansas, and New <br />Mexico. <br /> <br />Between Canon City and Pueblo the river flows in a transitional <br />region between the high mountains and the eastet'n plains. <br /> <br />Downstream of Pueblo, the river flows east across the eastern <br />plains to the Kansas border. In this region the valley is <br />between one and three miles in width with relatively flat <br />slopes. The main tributaries of the Arkansas River are Fountain <br />Creek, St. Charles River, Apishaza River and Timpas Creek. <br />Normal rainfall precipitation in the Arkansas River Basin ranges <br />from approximately 12.5 inches per year in the lower elevations <br />to approximately 16.8 inches per year in the mountainous regions <br />(Reference 6). In the Timpas Creek Basin, normal annual <br />precipitaion is 12.5 inches. Maximum and minimum \,emperature, <br />extremes range in the study basins from about 110 F in the <br />lowlands to about .30or in the highlands. Vegetation in the <br />study basin consists of mesquite and willow bushes, with <br />occasional groves of cottonwoods and juniper bushes. In the <br />upper part of the basin, evergreens and aspen are predominant. <br /> <br />B. Study Reach Description <br />The ~tudy reach of this floodplain information report extends <br />from the upstream Umit of the Corps of Engineers study near <br />La Junta for approximately 15.5 miles upstream to Rocky Ford. <br />Two additional study areas include a 1.0 mile reach near <br />Manzanola and 1.7 mile reach near Fowler. The Timpas Creek Study <br />reach extends from the Arkansas Rivet' for a distance of 2.5 miles <br />upstream. The Arkansas River and Timpas Creek valleys are <br />genl!rally broad and flat. Along the Arkansas River the land <br />immediately adjacent to the river has heavy growths of trees and <br />brush interspersed with meadows and cultivated land. Timpas <br />Creek is bordered on both sides by cultivated lands. The towns <br />of Swink, Rocky Ford. Manzanola and Fowler are generally located <br />outside of the floodplains of the study streams and there is <br />generally little development at present in the floodplains. <br /> <br />A. Drainage Basin Characteristics <br />The Arkansas River originate a in the high mountains <br /> <br />along the <br /> <br />The portion of the Arkansas River 3asin under consideration in <br />this study has its downstream limit at the upstreanl limit of the <br />1977 Corps of Engineers Study. The upstream limit on the <br />Arkansas is approximately 550 ft. upstrea... of Fowler, Colorado. <br />The total study reach on the Arkansas River is 18.5 miles. Also <br />included in this rl'port is a 2.5 mile reach of Timpas Creek, <br />starting at its confluence with the Arkansas River and extending <br />upstream. <br /> <br />III. STUDY AREA DESCRIPTION <br /> <br />.5- <br /> <br />,', <br />