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RULE 2 PERMITS <br />As part of the investigations begun in 2004, WMC also identified ten springs and seeps, seven of which <br />had been previously identified by JBR Environmental Consultants (JBR) in 1998. Tetra Tech (dba; <br />Maxim Technologies) and Cedar Creek Associates also identified seeps and springs within the general <br />area along Collom Gulch, Little Collom Gulch, Jubb Creek (mainstem and both forks), Straight Gulch, <br />upper Wilson Creek, and areas in between. A total of 46 seeps and springs were observed during the <br />inventory, of which 33 fell within the Collom, Little Collom, or Jubb Creek drainages that may be <br />affected by the mining. Those spring and seep monitoring locations applicable to the Collom permit <br />expansion area are summarized in Table 2.04.7-47, and monitoring results are summarized in Table <br />2.04.7-49. Spring and seep monitoring locations are depicted on Map l OB. <br />Surface Water Quality — Several surface water quality investigations have been performed in the general <br />area, in conjunction with the water quantity measurements discussed above. The water quality aspects of <br />these investigations are discussed in the following paragraphs. <br />The USGS collected water quality data at several area stream gages as early as 1947. Data from those <br />gages are summarized in Table 2.04.7-45. The USGS discontinued water quality monitoring at the last of <br />these stations in 1992. <br />Engineering Science (ES) 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 over a 12 -month span from August 1984 through July 1985. <br />Surface water monitoring locations were established in Good Spring Creek, Wilson Creek, and Taylor <br />Creek as part of these studies. <br />Colowyo monitored baseline surface water quality in stream water, springs, and seeps at selected <br />locations from September 1996 to September 1997 (Jubb Creek and forks only), December 2004 through <br />May 2006 and March of 2012 through April of 2015. Monitoring was performed in Jubb Creek, Collom <br />Gulch, Little Collom Gulch, Straight Gulch, and nearby areas during this period. Findings of those <br />studies are discussed in the detailed information below. Surface water monitoring locations applicable to <br />the Collom permit expansion area are summarized in Table 2.04.7-46, and monitoring results are <br />summarized in Table 2.04.7-48. Spring and seep monitoring locations applicable to the Collom permit <br />expansion area are summarized in Table 2.04.7-47, and monitoring results are summarized in Table <br />2.04.7-49. Surface water monitoring locations, including springs and seeps, are depicted on Map l OB. <br />Surface Water Use — Surface water is used extensively in the broader stream valleys of the area. Surface <br />water consumption is predominantly associated with irrigation of agricultural lands. Surface water <br />withdrawals in Moffat, Rio Blanco, and Routt Counties totaled 690.50 million gallons per day (mgd) in <br />2000 (USGS 2004). About 97 percent of the surface water withdrawal volume (668.66 mgd) was used <br />for irrigation. The irrigated acreage totaled 117,560 acres. Public water supply (1.2 percent) and <br />thermoelectric power generation (2.0 percent) account for the remaining surface water withdrawals. In <br />Moffat County alone, irrigation of 36,370 acres claimed 92.8 percent of the 207.42 mgd total surface <br />water withdrawal, while public supply and power generation claimed 1.8 percent and 5.4 percent, <br />respectively. <br />All of the major streams are over -appropriated, and therefore, many of the surface water rights are <br />inactive (CDM, 1985b). Large storage reservoirs are often constructed to capture spring runoff and <br />facilitate irrigation of fields in the summer months when natural flows are diminished. <br />Collom — Rule 2, Page 30 Revision Date: 4/7/17 <br />Revision No.: RN -07 <br />