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PERMFILE67666
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PERMFILE67666
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Entry Properties
Last modified
8/24/2016 11:13:23 PM
Creation date
11/20/2007 9:59:38 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981013
IBM Index Class Name
Permit File
Doc Date
7/3/2003
Section_Exhibit Name
Section 2.04 Site Description and Land Use Information
Media Type
D
Archive
No
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<br />Surface Water Monitoring <br />i WFC has been gathering stream flow and water quality <br />baseline data from the Purqatoire River and side-canyon areas <br />since February, 1984. This data has been gathered as per the <br />requirements of permit stipulations and the previous year's data <br />is presented in Exhibit 10, Annual Hydrology Report. <br />During the spring of 1984, flume stations were <br />constructed and Stevens Type F continuous recorders were <br />calibrated and placed in operation on Apache and Santistevan <br />Canyons on April 5 and 20, respectively. These stations were <br />maintained for a period of 14 months until sufficient data was <br />collected to differentiate seasonal flow variations. Also, <br />Ciruela Canyon stream flow has been monitored quarterly at two <br />surface stations, one above the Golden Eagle Mine and one at the <br />confluence with the Purgatoire River below the Golden Eagle <br />• Mine. Baseline studies of Lopez, Wet and Cherry Canyons began <br />in July, 1988. All data collected from these canyons is <br />summarized below. <br />Santistevan Canvon. During the flume monitoring period <br />of April, 1984, through August, 1985, flows ranged from 0.014 to <br />greater than 30.4 cfs with an average 24 hour mean of 0.096 cfs. <br />Monthly visits to the station began again in January, 1989, and <br />showed that the station was dry during the winter and spring <br />period. Runoff calculations indicate an annual discharge of 148 <br />acre-ft. The majority of this runoff was recorded during the <br />summer months in the form of heavy localized thunderstorms. <br />These storms produced extreme spikes in the hydrograph, two of <br />which exceed the recording limits of the flume station. A <br />relatively constant flow was observed during the fall and winter <br />seasons dictated by snow and the freeze-thaw cycle, and limited <br />vegetation growth eliminating evapotranspiration water loss. <br /> <br />2.04-22 (Revised 09/01/89) <br />
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