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FLOOD03149
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FLOOD03149
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Last modified
1/25/2010 6:26:27 PM
Creation date
10/4/2006 11:29:29 PM
Metadata
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Floodplain Documents
County
Gilpin
Community
Central City
Stream Name
Eureka and Nevada Gulches
Basin
South Platte
Title
FEMA LOMR Application Hydrologic and Hydraulic Study
Date
10/1/1991
Prepared For
Central City
Prepared By
RMC
Floodplain - Doc Type
Floodplain Report/Masterplan
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<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 />I <br />I <br />I <br />I <br /> <br />Goldhill, all in vain. Due to lack of specific data, the NOAA <br />Atlas II precipitation values were used as discussed above. <br /> <br />2. Appendix "B", Watershed Data <br /> <br />Watersheds were delineated based on 40' contours from a 1"= 2,000' <br />USGS quadrangle map, with additional clarification within City <br />1 i mi ts obta i ned from a 2' contour map at 1 "=100' prepared by Ray <br />and Associates in 1975 and by field reconnaissance to determine <br />effects of urbanization on flow patterns. Areas were determined by <br />planimeter. (See Exhibit "C".) <br /> <br />Time of concentrations and lag times were obtained by use of TR-55 <br />and NEH-4. <br /> <br />Experience by the author has indicated that the SCS runoff curve <br />number. (CN) selection is the most critical of all hydrological <br />parameters. For typical watersheds, percentage increases up and <br />down individually applied to basin area, time of concentration, <br />precipitation amount, and CN values indicate that the CN value is <br />approximately twice as sensitive as precipitation changes, which in <br />turn is approximately 2 and 3 times more sensitive than basin area <br />and time of concentration, respectively. Accordingly, much effort <br />was placed on CN selection. <br /> <br />An SCS soil survey has not been prepared for Central City area, nor <br />has the USFS prepared or contracted for a survey to be performed. <br />However, detailed soil information has been obtained for the <br />Dorothy Lee Placer area by Empire Laboratories in conjunction with <br />a study for a proposed water supply reservoir. (See Reference No. <br />7 in the Bibliography, and Appendix "B" for excerpts of report.) <br />The report indicates that topsoil is silty and underlaid with silty <br />sand. Soil overburden above bedrock is generally ample to <br />eliminate bedrock as a factor in CN selection. <br /> <br />5 <br /> <br /> <br />The report is for site specific soils. However, observation of <br />soils throughout the entire watershed at depths to 6 inches <br />indicate little variance from the silty sandy soil found in the <br />report. The soil textures fall into the hydro 1 ogi c soil group <br />(HSG) of B or better. A hydrology report for Eureka Gulch <br />watershed above the Dorothy lee Placer was also previously approved <br />by the office of the State Engineer which classified the HSG as B. <br />(See Reference No.8 in the Bibliography.) The HSG was assumed to <br />be B in this study. <br /> <br />The antecedent runoff condition (ARC), formerly called the <br />antecedent moisture condition, was assumed to be average, or <br />condition II. <br /> <br />Five (5) surface conditions exist in the watersheds. These are <br />forested, range, graded, impervious, and commercial areas. <br /> <br />Forested area classification in TR-55 is based on foliage type, and <br />should not be confused with "woods", which refers to orchards. <br />(See NEH-4.) Central City area forests fit into the oak/aspen <br />category of arid and semi-arid rangelands. <br />
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