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1987-12-01_PERMIT FILE - C1981017 (94)
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1987-12-01_PERMIT FILE - C1981017 (94)
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Last modified
1/4/2021 9:33:14 AM
Creation date
5/15/2012 10:21:42 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981017
IBM Index Class Name
PERMIT FILE
Doc Date
12/1/1987
Doc Name
Coal Refuse Facility Driainage Control Plan
Section_Exhibit Name
Chapter II Attachment 5 to Appendix II-B-7 (11-B-App. 7 Att.5)
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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II <br /> lying Mesaverde Formation outcrop north of the area at higher <br /> elevations. The ridges , formed by Mancos Shale , are locally <br /> covered by important accumulations of colluvial soils of un- <br /> known thickness. A large landslide has been identified north- <br /> east of the proposed waste disposal area. <br /> The waste disposal area is bordered on the south side by <br /> alluvial deposits of Coal Creek. <br /> 3. 0 GROUND WATER HYDROLOGY <br /> It can be expected that ground water will be encountered <br /> in two formations at or close to the proposed waste disposal <br /> site : <br /> o Ground water in Coal Creek alluvium. It is probable <br /> that continuous ground water exists in the alluvium of Coal <br /> Creek. As the Coal Creek alluvium is outside the area of <br /> interest, no studies have been made on this ground water. Coal <br /> Creek alluvium can be influenced by discharge of ground water <br /> from the outwash sediments. The valley of Coal Creek is lower <br /> than the outwash deposits north of it; the creek has locally <br /> i eroded the outwash deposits so that a discharge from them <br /> into the Coal Creek alluvium cannot be excluded. <br /> o Ground water in outwash deposits. It is reasonable to <br /> expect that ground water can be encountered in the outwash <br /> ideposits in both east and west valleys. Geotechnical mapping <br /> of the area above the east valley indicated the large land- <br /> slide with numerous wet spots and the apparent presence of <br /> ground water. This ground water will be discharged into the <br /> east valley; ground water can be expected to exist there. The <br /> west valley can be recharged by water from several creeks <br /> observed in higher reaches of the valley. <br /> No ground water has been observed in the bedrock forma- <br /> tions. The ridges on both sides of the disposal area are dry, <br /> and no springs have been observed there. <br /> 4. 0 GROUND WATER INVESTIGATION <br /> A total of three monitoringwells were installed lled within <br /> the project area to obtain baseline ground water data and to <br /> enable continued monitoring of ground water elevations and <br /> ground water quality. <br /> r 15 <br /> t GfOHYDRO CONSULTING.INC. <br />
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