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Many trace elements were consistently found to be near or below the detectable limits for all springs for the 2000 water yeaz. These same trace elements have historically been found to be below detectable limits. They aze aluminum, ammonia, arsenic, cadmium, copper, iron (both total and dissolved), lead, mercury, molybdenum, nitrite, nitrate, nitrate/nitrite, phosphate, selenium, and zinc. RESULTS -MONITORING WELLS FOR WATER YEAR 2000 Three groundwater monitoring wells were sampled during the 2000 water yeaz. The wells sampled are designated 17-B, 94-1, and 95-1. Well 17-B is 600' west of the corner of the northwest permit boundary within Cazbon Junction Canyon. Well 94-1 is located adjacent to the east edge of the south pit. Well 95-1 is located approximately 850 feet south- southwest of the future pit boundary. Well 17-B is located upgradient of any disturbance related to mining. Well 94-1 is located within the area disturbed by mining, and well 95-1 is located downgradient and outside the proposed coal mining disturbance. As such, these wells (94-I and 95-[) would be expected to show any changes resulting from nrining disturbance. These wells may also show changes to groundwater due to adjacent sand and gravel mining on Ewing Mesa. Each of the wells was sampled once during the 2000 water year. Sampling occurred during the third water yeaz quarter (June 8). Summaries of sampling data from the groundwater wells for the 2000 water yeaz are contained in Tables 3, 4, and 5. The depth to water in wells 17-B and 95-1 remained relatively consistent during the 2000 water year with a slight increase in depth to water for well 94-1 and a slight decrease in depth to water in wells 17-B and 95-1. In well 94-1, depth to water has fluctuated widely in the last four water yeazs. Between the fast and third calendar quarters of 1997, the depth to water in 94-1 increased from 22 to 64 feet. Between the first and second calendar quarters of 1998, the depth to water level returned to 22 feet from 64 feet. Between the fourth calendar quarter of 1998 and the second calendaz quarter of 1999, the depth to water level in well 94-1 again dropped, this time to 76 feet. During the second calendar quarter of 2000 the depth to water level returned to 31 feet. At this time there does not appear to be a definitive explanation for this occurrence. It is interesting to note this fluctuation, as no significant fluctuation in water level in the other monitoring wells has occurred either above or below the mine. Water temperature in the wells fluctuates regularly with the seasons. Water temperatures are lowest during the winter months and highest during the summer months. Temperature generally fluctuates most in the shallowest well (17-B) and least in the deepest well (95-1 j. Temperature ranges for the 2000 water year remained within those observed previously for the wells. The pH for all wells changed from slightly basic during the end of water year 1996 to slightly acidic at the beginnittg of water yeaz 1997. During this water yeaz (2000), the pH -5-