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<br />2.3 Principal Flood Problems <br /> <br />Historical accounts of flooding include references to several floods <br />in the study area. Information on past floods, as available in <br />newspaper files and other historical documents, is almost exclusively <br />concerned with the larger aspects of flooding on Fountain or Monument <br />Creeks. Major flooding probably included simultaneous flooding on <br />smaller streams as well. Reference to the smaller streams appears <br />only rarely in early newspaper accounts. Specific information of <br />the intensity, duration, and magnitude of the storms and flood <br />effects are generally lacking. <br /> <br />On the basis of available peak discharge data alone, the floods of <br />1864, 1866, and 1935 would be classified as major in destructive <br />capability. The May 1935 flood is the flood of record for Fountain <br />and Monument Creeks in Colorado Springs. The June 1965 flood on <br />Fountain Creek was primarily caused by Jimmy Camp Creek, which at <br />a point 4.5 miles above the Fountain Creek/Jimmy Camp Creek conflu- <br />ence had an estimated peak discharge of 124,000 cubic feet per <br />second (cfs). <br /> <br />The following summaries of floods were taken primarily from a U.S. <br />Geological Survey (USGS) publication (Reference 3) and from the <br />COE files. <br /> <br />June 10, 1864. The Colorado Springs Gazette of June 27, 1864, in <br />a series of articles on early happenings refers to the flood of <br />1864 as follows: <br /> <br />There had been several thundershowers and the creeks were <br />somewhat swollen, though not so much as to cause any apprehen- <br />sion. But by 4 o'clock . . . a heavy cloud came up over <br />Cheyenne Mountain and the sky gathered darkness until nearly <br />sundown, when rain and hail began to fall in tremendous torrents. <br />The rain came down, not in drops but in floods, the <br />hail consisted of huge lumps of ice, some of them over 3 <br />inches in diameter1 the whole surface of the country was <br />flooded as though it were a vast lake, and in some of the <br />ravines the water rushed along in torrents 20 or 30 feet <br />deep. The storm continued in full violence until about 9 <br />o'clock. The area of the storm was confined within a radius <br />of 3 or 4 miles. <br /> <br />, <br /> <br />May 20, 1878. Although the few available precipitation records <br />for 1878 indicate no general storm, a cloudburst near Palmer Lake <br />caused a flood that was reported by the Rocky Mountain News of May <br />20, 1878, as follows: <br /> <br />Monument and Fountain Creeks swept out bridges. El Paso <br />County Losses very heavy, caused by cloudburst in valley <br />near Divide, followed by hail. <br /> <br />9 <br />