Laserfiche WebLink
<br /> TABLE 4 <br /> HIGHEST TEN RECORDED FLOWS IN ORDER OF MAGNITUDE <br /> FOUNTAIN CREEK IN PUEBLO. COLORADO <br /> Estimated <br />Order Gaoe Heiohts Peak <br />Number Date of Crest Staoe Elevation Discharoe <br /> feet feet c.f.s. <br />1 June 17, 1955 19.00 4,5B2.5 47,000 <br />2 May 30, 1935 * 35,000* <br />3 June 4, 1921 * 34,000* <br />4 July 10, 1945 9.50 4,573.0 17,800 <br />5 Aug. 25, 1945 9.00 4,572~5 15,500 <br />6 Aug. 4, 1944 8.51 4,672.0 12,900 <br />7 Oct. 3, 1923 5.BO 12,000 <br />B Aug. 23, 1946 8.00 4,571.5 11,BOO <br />9 July 30,1951 7.95 4,571.4 11,500 <br />10 AU9. 6, 1955 7.90 4,571.4 11,500 <br /> <br />*Gage was not used to make measurements; 35,000 and 34,000 c.f.s. <br />are slope-area measurements. <br /> <br />Flood Occurrences <br /> <br /> <br />Ana1yeis of climatological data and inspection <br /> <br /> <br />of the flood history for the Arkansas River subbasin above John <br /> <br /> <br />Martin Dam show that the most severe flood-producing storms occur <br /> <br /> <br />during the late spring or summer months. The spring season is the <br /> <br /> <br />transitional period between the occurrence of instability and fron- <br /> <br /> <br />tal activity and is subject to storms caused by both types of ac- <br /> <br /> <br />tivities or a combination thereof. Also, the movement and interac- <br /> <br /> <br />tion between airmasses during these seasons are more pronounced. <br /> <br /> <br />This may result in heavy spring snow storms in the higher elevations <br /> <br /> <br />Or in high intensity rains during the spring. These storms and the <br /> <br /> <br />physical features of the watershed can produce the rapid concen- <br /> <br /> <br />tration of runoff that characterizes flash floods of high peak <br /> <br /> <br />flows, small volumes, and short durations. <br /> <br />22 <br />