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RULE 2 PERMITS <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 />10). A total of 59 seeps and springs were observed during the inventory. Seeps and springs are identified <br />in Table 2.05.6-1 and -2. Four springs within the general area appeared perennial: one on a western <br />tributary to Wilson Creek (WCS-1), one on the eastern tributary to Wilson Creek (WCS-3), and two on <br />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 discharge 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 mining. Some of these correspond with springs identified by CDM. Colowyo identified <br />several additional springs in the mining impact areas. The spring information from all sources was <br />consolidated and 21 spring sampling locations were identified to the Division for the South Taylor impact <br />area. The Division approved of the selected spring locations in 1999. Five springs in the Lower Wilson <br />area were also identified and are 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 a magnesium -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 a magnesium -sulfate <br />water type. TDS values ranged from less than 1,000 mg/L to nearly 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 2,130 mg/L (CDM, 1985b). TDS concentrations were also <br />inversely related to stream discharge. Water quality in Taylor Creek is characterized by generally low <br />concentration of major ions. The water is primarily a calcium -bicarbonate type, with low TDS ranging <br />from 472 to 500 mg/L (CDM, 1985b). <br />South Taylor/Lower Wilson — Rule 2, Page 25 Revision Date: 4/7/17 <br />Revision No.: RN -07 <br />