Laserfiche WebLink
<br />I <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br />I <br /> <br />7 <br />- ~ - <br /> <br />of the Blue River in the Breckenridge area lasts for several <br />weeks and takes many days to reach its peak discharge. The <br />beginning of the snowmelt is around the first part of r1arch <br />and the hydrograph does not peak until the middle of June. <br />For the Breckenridge area,~the-~ate of average peak discharge <br />in the Blue River is JU~nd has an average buildup of <br />approximately 46 days prior to the date of peak. <br /> <br />STORM OF RECORD <br /> <br />'1 <br /> <br />The peak discharge recorded by the u.S. Geological Survey <br />on the Blue River near Dillon for the 64 years of record was <br />1250 cfs and occurred on June 17, 1965. The flow was a com- <br />bination of snowmelt and, according to local residents in the <br />area, a high intensity thunderstorm of small areal distribution <br />centered in a tributary basin above the town. Examination of <br />the hydrograph for this stolm period, which is shown in Figure <br />1 as well as preciPitationldat~)recorded at Breckenridge and <br />Dillon, permits_~nalYSiS~Of the peak discharge. <br /> <br />The Breckenridge guage recorded several days during which <br />precipitation fell on the basin in a two week period preceding <br />the date of the discharge. Because of the limited data <br />on the type of areal distribution of precipitation that fell <br />in that time period it is possible that the Breckenridg~ga~ <br />'-_ 0_ <br />recorded rainfall in the lower portion of the basin and that <br />snow could have fallen in the higher elevations. Comparison <br />of the two weeks of rainfall with the hydrograph of the gage <br />in the Blue River for the same period of time reveals no <br />-- <br />significant a1ter~:ions, in, the m~a~ ~a~~~ di~~h..arge. The <br />-discharge of the Blue River continued to rise at a relatively <br />steady rate. <br /> <br />Interviews with local residents in the area state that <br />the storm of June 1965 was centered over Spruce Creek, a small <br />tributary above the town of Breckenridge. Although no official <br />recording gage was centered in the tributary, residents claim <br />that approximately 2 to 3 inches fell in a very short time <br />