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<br />-- <br /> <br />I <br />I <br />I <br />1 <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />4.3 STREAMFLOW <br /> <br />Stream gage and discharge records are available from the U.S. Geological Survey <br />(USGS) for three stations within the Fountain Creek drainage basin study and for <br />one station located downstream of the study boundary. Gage 07103700 (the Manitou <br />Gage) is located near the west ci ty 1 imits of Colorado Spri ngs, approximately one <br />mile downstream of Sutherland Creek, and has a period of record from April 1958 <br />to the current year. The peak flow rate for this period of record is a discharge <br />of 2,630 cfs, on August 4, 1964. Natural flows upstream of this station are <br />affected by storage reservoirs, power generation developments, diversion for <br />irrigation and municipal use, and at certain times, transbasin diversion from the <br />Beaver Creek drainage and transmountain diversions from the Colorado River Basin. <br /> <br />Gage 07105500 (the Tejon Gage) is located 31 feet upstream from the bridge on <br />Nevada Avenue, approximately 1.3 miles downstream from the confluence of Monument <br />and Fountain Creeks. The gage has a period of record from October 1921 to <br />September 1924, and January 1976 to the current year. The peak flow rate for <br />this period of record is a discharge of 5,300 cfs, on July 29, 1978. Natural <br />flows upstream of the gage are affected by storage reservoirs, power <br />developments, groundwater withdrawals, diversions for irrigation and municipal <br />use, return flows from i rri gated areas and discharges from sewage treatment <br />facil ities. <br /> <br />Gage 07105530 (the Janitell Gage) is located on the upstream side of the newly <br />constructed Janitell Road bridge. The gage has a period of record from October <br />1989 to September 1990. This gage was not considered in the gage analysis due <br />to the limited period of recorded data. <br /> <br />Gage 07105800 (the Security Gage) is located downstream of the study boundary at <br />Securi ty. The gage is on the upstream side of Carson Road bri dge and has a <br />period of record from October 1964 to the current year. The peak flow rate for <br />this period of record is a discharge of 25,000 cfs, on July 24, 1965. Natural <br />flows upstream of the gage are affected by reservoirs, power generation <br />developments, diversion for irrigation and municipal use, return flows from <br />irrigated areas and flows from sewage treatment facilities. Refer to Figure 4.3- <br />1 (Volume II) for gage locations. <br /> <br />The positioning of the Manitou, Tejon and Security gages and their period of <br />record permits them to be used as hydrologic index locations for the purposes of <br />the computation of design hydrology. <br /> <br /> <br />4.4 FLOOD HISTORY <br /> <br />Historical documents, newspaper files, publications by the U.S. Geological Survey <br />and the Colorado Water Record were utilized as sources of past flood damage and <br />flood discharge estimates within the drainage basin. Documentation on past flood <br />events from historical sources indicate that several floods have inundated and <br />inflicted damage in some portions of the study area since 1864. Historical <br />records on flooding are generally informative; however, specific information on <br />intensity, duration, and magnitude of the storms and corresponding floods are <br />lacking. <br /> <br />4.0-3 <br />