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flow. Conductivity of the water was stable, ranging fran 629 to 720, while <br /> pH ranged from 7.6 to 7.9. Use of the water is limited to livestock and <br /> wildlife watering. <br /> Spring #13: Apache Canyon (Table 3) . This seep originates fran the <br /> interface of shale and sandstone. Flora was measured on 7 of the 9 samplings <br /> ranging fran <1 to 3 gpm. The flaw was absorbed into the alluvium within 50 <br /> yards of the source during each of the 7 observations. As a result, this <br /> seep is not a significant source of surface flaw. Water quality <br /> measurements of conductivity range from 700 to 721, while pH ranged fran 7.3 <br /> to 7.7. Use of the seepage is limited to livestock and wildlife watering. <br /> Spring #14: Apache Canyon (Table 4) . This is a USGS developed spring <br /> originating fran an upper coal seam or interface between coal and shale or <br /> sandstone. Flow could not be measured because of the associated pond at the <br /> site, however, water levels in the pond appeared to be constant over the <br /> monitoring period. This spring does not contribute to Apache Canyon stream <br /> flow because an Embankment creating the pond separates the two. <br /> Conductivity ranged fran 562 to 739, while pH ranged from 7.4 to 8.9. Use <br /> of the water is limited to livestock and wildlife watering. <br /> Spring #15: Ciruela Canyon (Table 5) . Spring #15 is a minor area of <br /> seepage fran the interface of shale and sandstone below a coal seam outcrop. <br /> No flow was measured during the monitoring period. Water quality was <br /> measured on one occasion with conductivity at 1054 and pH at 6.7. This <br /> spring is not significant to surface flow and only has value for livestock <br /> and wildlife watering in the spring of the year. <br /> Spring #16: Ciruela Canyon (Table 6) . Flow originates from the <br /> interface of shale and sandstone and was measurable on 7 of the 9 samplings <br /> ranging fran <1 to 3 gpm. On all occasions flow was absorbed into the <br /> alluvium within 100 yards of the source and does not appear to contribute <br /> significantly to surface flow. Conductivity and pH ranged fran 780 to 984 <br /> and 6.4 to 8.0, respectively. The spring does provide livestock and <br /> wildlife water, however, is not that important due to the location of a <br /> stock pond 200 yards upstream. <br />