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<br />14_ <br /> <br />. <br /> <br />16. <br /> <br />16_ <br /> <br />17_ <br /> <br />18. <br /> <br />19. <br /> <br />20. <br /> <br />21. <br /> <br />. <br /> <br />John F. Osborn, Determining Stream Flows from Geomorphic Para. <br />meters, A$CE Irrigation and Drainage Journal, Vol. 100. <br />No.IR4(1974}. <br /> <br />Charles Robinson & Associates, Inc., National Soils Services, <br />Inc., 1972 Geotechnical Investigation,Vol.I,Preliminary <br />Geologic and Engineering Investigation, Eagle-Piney <br />Project (I973). <br /> <br />. <br /> <br />Arthur Judson, The Weather and Climate of a High Mountain Pass in <br />the Colorado Rockies. U.S. Forest Service Research Paper <br />RM-16(1965). <br /> <br />ArdenO.Haeffner,DailyTemper<lturesandPrecipitationforSub_ <br />alpine Forest, Central Colorado, U.S. Forest Service Research <br />Pa~er RH.8D (1971). <br /> <br />Snow Frequency Analysis for Colorado and New Mexico Snow Courses. <br />U.S. Soil Conservation Service (I973). <br /> <br />"Design of Small Dams",SecondEdition, U.S. Bureau of Reclamdtio n, <br />1973. <br /> <br />- <br /> <br />"Water Resources Data forColorado-Part I,SurfaceWater <br />Records", Water Supply Paper (WsP) 1313 and WSP 1733, <br />U.S. Geological Survey. <br /> <br />"Rainfall Frequency Atlds of the United States. TechniCdl Paper <br />40", U.S. \o/eatherBureau, 1961. <br /> <br />. <br /> <br />GENERAL NOTES <br />FOR THE PLATES <br /> <br />1. The Gore Creek streambed stationing begins at the con- <br />fluence of Gore Creek with the Eagle River and is expressed <br />in 100 foot stations. <br /> <br />2. In numerous locations, the 10 year and 100 year recurrence <br /> <br />interval floodplain limits coincided so closely that presen- <br />tation on the same plate would reduce overall legibility. <br />The flow depths at the reference points for the 10 year <br />recurrence interval discharge are presented on Table III~2-B. <br /> <br />3. The confluence of Black Gore Creek with Main Gore Creek is very <br />poorly defined due to braiding of both channels. The exact <br /> <br />confluence will vary from year to year depending on the erosion <br />or meandering of the several channels. For the purpose of <br /> <br />this study, station 65.1 was chosen ~5 the confluence ?nd <br /> <br />separate stationing continued a short distance up both Main <br />Gore and Black Gore Creeks. <br />