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PERMFILE118331
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Entry Properties
Last modified
8/24/2016 10:14:01 PM
Creation date
11/25/2007 5:05:04 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Revision
Doc Date
12/2/2004
Doc Name
Exhibit 55A Certification Stream Channel Parameter & Changes Due to Mining Induced Subsidence
Type & Sequence
PR10
Media Type
D
Archive
No
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• Stream Channel Paremetere <br />Exhibit 55A and Changes Due to Mining•Induced Subsidence Page 4 <br />of 630 AF per squaze mile; the runoff magnitude is significantly affected by the higher <br />precipitation values at higher elevations in the drainage basin. <br />Analyses of water yield by William Lorah of W WE for the Division No. 4 Water Court approved <br />water augmentation plan, indicated that typical annual water yields for tributaries of Dry Fork <br />were approximately 200 AF per square mile per year. This value compares favorably with the <br />yield estimate of 160 AF per square mile per yeaz based on the U.S. Geological Survey (USGS) <br />regional regression equations (USGS 1985). <br />The 1936 through 1947 and 1985 through 2002 periods of gaging flow on Minnesota Creek show <br />an average annual yield for 41.3 squaze miles of 385 AF per square mile. <br />For the purpose of annual average sediment yields for the subject basins, WWE and Mr. <br />Pemberton have concluded that an appropriate (i.e., conservative) mean annual runoff for the <br />• subject basins of 475 AF per yeaz should be adopted, even though site-specific data for the basins <br />would likely indicate a mean annual runoff of less than 475 AF per year per square mile. The <br />adopted value represents a high mean annual runoff for use in conservative sediment and channel <br />stability studies. For water rights purposes, the average yeaz yield estimate of 200 AF per year is <br />suitable, as approved by the Colorado Water Court in 1986. <br />Peak Runoff Rates <br />Peak rates of storm runoff from rainfall and snowmelt events were defined for three return <br />frequencies: 2-, 10., and 100-yeaz events. <br />These dischazges aze based on statisfical evaluation of peak daily flow data collected by MCC in <br />the permit azea since 1978, study of the long-term published records for the North Fork at <br />Somerset, and statistical evaluation of published streamflow data for basins in the vicinity of <br />West Elk Mine. Special evaluations were made of the Lick Creek, Sylvester Gulch, and Horse <br />Creek basins using the USGS peak rate of runoff computational procedure applicable to small <br />. basins in the Colorado mountainous azea (USGS 1985). <br />831-032.620 Wright Water Engineers, Inc. <br />
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