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2013-10-02_PERMIT FILE - C1981019A (3)
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2013-10-02_PERMIT FILE - C1981019A (3)
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Last modified
8/24/2016 5:31:59 PM
Creation date
10/18/2013 8:51:20 AM
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Template:
DRMS Permit Index
Permit No
C1981019A
IBM Index Class Name
Permit File
Doc Date
10/2/2013
Section_Exhibit Name
Rule 2 Permits -ST
Media Type
D
Archive
Yes
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RULE 2 PERMITS <br />• flows occurring during August through September ranged from 0.01 to 0.02 cfs, whereas high flows in <br />May measured 1.87 cfs (CDM, 1985b). The drainage was dry during November. The flow data compiled <br />by CDM for Good Spring Creek, Wilson Creek, and Taylor Creek correlates with the data compiled by <br />the USGS and Brant Dennis. <br />As part of the 1985 investigation, CDM also surveyed seeps and springs within the general area along <br />Good Spring Creek, the West Fork of Good Spring Creek, and Wilson Creek, and areas in between (Map <br />l0A). A total of 59 seeps and springs were observed during the inventory. Seeps and springs aze <br />identified in Table 2.05.6-1 and -2. Four springs within the general azea appeared perennial: one on a <br />western tributary to Wilson Creek (WCS-1), one on the eastern tributary to Wilson Creek (WCS-3), and <br />two on tributaries to Good Spring Creek (WFS-2, JCS-1). The seeps and springs were monitored for field <br />parameters on a monthly basis, and a single full-suite sample was collected at each location in May 1985. <br />The monitoring data illustrate that springs contribute up to 1.9 cfs to surface flows in the West Fork of <br />Good Spring Creek, and about 1 cfs to surface flows in the mainstem of Good Spring Creek during peak <br />flow periods (CDM, 1985b). Contributions to surface flows from spring dischazge during baseflow <br />periods were much less, ranging from 0.03 cfs to 0.06 cfs in the West Fork of Good Spring Creek, and <br />0.03 cfs in the mainstem (CDM, 1985b). <br />Springs were also inventoried by JBR (1997). JBR identified 29 seeps and springs within areas that could <br />be impacted by proposed mining. Some of these correspond with springs identified by CDM. Colowyo <br />identified several additional springs in the mining impact areas. The spring information from all sources <br />was consolidated and 21 spring sampling locations were identified and proposed to the CDMG for the <br />South Taylor impact area. The CDMG approved of the selected spring locations in 1999. Five springs in <br />the Lower Wilson area were also identified and aze presented in this application. <br />• Surface Water Quality -Water quality data for streams and springs that is relevant to this permit <br />revision are summarized in tables 2.04.7-30, 2.04.7-34, and 2.04.7-35. Several surface water <br />investigations have been performed in the general area. These are discussed in the following paragraphs. <br />Engineering Science measured parameters in area streams and springs from 1978 through 1982 (ES, <br />1982). The report concluded that Taylor, Good Spring, and Wilson creeks all have variable water quality <br />that depends on season. Background levels of metals indicate acute and chronic toxicity to aquatic life in <br />all drainages. It further concluded that levels of metals in surface water may affect agricultural uses, and <br />that high metal and sulfates may preclude the use of surface water for potable water supplies. <br />CDM investigated surface water quality of the streams in the general area covering a 12-month span from <br />August 1984 through July 1985. Surface water monitoring locations were established in Good Spring <br />Creek, Wilson Creek, and Taylor Creek as part of these studies. Generally, the surface water in Good <br />Spring Creek is amagnesium-sulfate type with calcium and bicarbonate also occurring in significant <br />concentrations. The TDS ranges from 713 mg/L to 1,500 mg/L (CDM, 1985b). TDS concentrations <br />were inversely proportional to flow; TDS was highest during low flow conditions in the stream, primarily <br />occurring during the winter months. <br />Most of the springs sampled in the Good Spring Creek drainage by CDM were amagnesium-sulfate <br />water type. TDS values ranged from less than 1,000 mg/L to neazly 5,000 mg/L (CDM, 1985b). Springs <br />sampled in the Wilson Creek drainage were lower in TDS, and had higher proportions of calcium and <br />bicarbonate. <br />Water quality in Wilson Creek is a mixed cation, mixed anion type, with sodium and chloride the <br />. dominant ions in the fall and winter months, and calcium, magnesium, and sulfates the dominant ions in <br />the spring. TDS ranged from 554 mg/L to 2,li0 mg/L (CDM, 1985b). TDS concentrations were also <br />South TaylodLower Wilson -Rule 2, Page 44 RaVI$ion Date: 3~30~07 <br />Revision No.: PR-02 <br />
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