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5.0 Geotogic and Hydrogeologic Setting of the Disposal Area <br />' The Lyons quarries are located entirely within the Upper Cretaceous Niobrara <br /> Formation. This Formation has a total thickness of about 400-feet and consists <br /> of two members, the Smokey bill Shale Member and the Fort Hays Limestone <br /> Member. The Smokey Hill Shale is a fissile, calcareous shale and the Fort Hays <br /> Limestone is athick-bedded limestone. In the quarry area the bedding planes <br /> dip to the east -southeast at about 10-15 degrees. C-Pit was excavated into the <br /> Fort Hays Limestone and the pit is underlain by the Carlile Shale, Greenhorn <br /> Limestone, Graneros Shale and Mowry Shale. These rock units consist of <br /> interlayered siltstone, claystones, limestones and shales. This sequence is <br />I about 500-feet thick and is underlain by the Lower Cretaceous Dakota Group. C- <br /> Pit is about 20 acres in size and 70-ft deep. <br />i - Ttie area surrounding C-Pit has been heavily disturbed by mining. Mining and <br />^ subsequent backfilling with overburden has occurred west and east of C-Pit, <br /> pursuant to the reclamation plan approved in M-77-208. <br /> <br /> North and east of C-Pit are alluvial deposits of the St. Vrain Creek The sand and <br /> gravel deposits are 25-30 feet thick and come into contact writh the sedimentary <br />rocks surrounding C-pit approximately 1,000 feet away at the closest point. <br /> There is absolutely no contact between the disposed CKD and the alluvial <br /> deposit. The CKD disposal mass is entirely contained within the sedimentary <br />1 rocks described above, <br /> Significant surface water bodies in the area, and the approximate distance from <br />osal area in C <br />Pit are as follows: <br />the CKD dis <br /> p <br />- <br /> St. Vrain Creek - Approximately 4700' at the closest point <br />Foothills Reservoir - Approximately 4200' at the closest point <br /> A-Pit Reservoir - Approximately 2000' at the closest point <br /> (A-Pit Reservoir is an approved water storage facility on Southdown <br /> property and within the M-77-208 permit boundary. The water is <br /> used for the cement plant.) <br /> Swede Ditch - Approximately 25' at the closest point <br /> Boulder Feeder Canal - Approximately 360' at the closet point <br /> The Swede Ditch which runs along the west rim of C-Pit was all enclosed in a 4- <br /> foot diameter corrugated steel pipe in 1998 in preparation for conversion of C-Pit <br /> from active quarry to CKD storage. All the pipe joints were sealed. The Boulder <br /> Feeder Canal is approximately 360-feet west and 9.5-feet higher (elevation <br /> difference from the bottom of the canal compared to the rim of C-Pit) than the rim <br /> of C-Pit. This eliminates the possibility of gravity flow from C-Pit to the canal. <br /> Runoff from the disposed CKD can not escape C-Pit and is entirely contained <br /> within the pit. C-Pit CKD storage has been designed and situated to eliminate <br /> the potential for leachate seepage into agricultural water canals now and in the <br /> future. <br />12 <br />