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APPCOR12198
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APPCOR12198
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Last modified
8/24/2016 6:32:33 PM
Creation date
11/19/2007 2:27:44 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981020
IBM Index Class Name
Application Correspondence
Doc Date
4/21/1981
Doc Name
MUNGER CANYON PERMIT APPLICATIONFN C-020-81
From
MLR
To
SHERIDAN ENTERPRISES INC
Media Type
D
Archive
No
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<br />~,.ater is encountered in the operation, the applicant should specify the <br />monitoring methods, frequency, and parameters to be analyzed for. Para- <br />meters should be determined in consultation with the Division. Also, <br />water quality analyses for the alluvial wells should include all those <br />parameters as required by the Division (See Appendix A). <br />3. The applicant should identify the potentiometric surface of any known <br />aquifers in the area, along with known uses of water in the aquifers <br />(including discharge/pumping rates). The potentiometric surface of each <br />aquifer should be clearly depicted on an appropriate map. This includes <br />the Cameo Coal Seam, which is unclearly depicted on Figure 4.9-1. If <br />any aquifers are noted to occur above the coal seam to be mined, provisions <br />must be made for monitoring them. <br />9. According to Figure 2.3-5, there is only one ground water monitoring <br />station (G-1) depicted on Salt Creek. On page 4-16 of the text, it is <br />stated that "...a total of six monitoring wells were installed (Figure <br />4.2-2)." Figure 9.2-2 has no legend and it is difficult to determine <br />which of the holes listed are the monitoring stations. Therefore, the <br />applicant should clearly show, on an updated map, where the ground water <br />monitoring stations on Salt Creek are located. <br />5. A11 drill logs submitted in the application are for drillholes that <br />were dry. The Division requests all additional drill logs, particularly <br />for holes where ground water was encountered. <br />6. Figure 9.4-1 depicts the ,potentfematsic surface for the Cameo Coal <br />Seam; however, all data concerning water levels are obtained from <br />exploration boreholes. Boreholes are open the entire length of the <br />drillhole to receive inflow of ground waters from all ground water <br />producing zones. Therefore, water levels monitored in the drill holes <br />may not be representative of the potentiometric surface for the Cameo <br />ground water system. Rather, the water levels observed are more likely <br />influenced by water producing zones above the Cameo seam. Sheridan <br />Enterprises must discuss the adequacy of water level information submitted <br />thus far. If sufficient rationale is not provided, the applicant will <br />likely have to case the boreholes so specific zones can be monitored <br />(such as the Cameo Coal Seam) in order to adequately define the ground <br />water system. <br />7. Several perched water zones were also identified by the applicant. <br />All geophysical logs submitted thus Far indicate that the boreholes <br />extend down to the coal seam. It is our understanding that during <br />drilling the first water producing zone can be reasonably located (if <br />drilling is done with air). Deeper water producing zones (where an <br />upper saturated zone was encountered) can only be detected by the <br />driller if significantly more water is encountered. Therefore, the <br />Division requests an explanation of how the upper perched zones were <br />located and how they distinguished from other saturated zones if more <br />than one water producing zone was encountered in the same hole. The <br />locations of the perched zones should be specified and a determination <br />must be made if the "perched" zones can be correlated to determine their <br />areal extent. <br />8. The Division also requests an explanation of how boreholes were <br />determined to be dry, particularly when the resistivity logs were <br />measured for the hole. <br />(3) <br />
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