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GENERAL31745
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Last modified
8/24/2016 7:54:42 PM
Creation date
11/23/2007 7:04:41 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1983058
IBM Index Class Name
General Documents
Doc Date
11/1/1983
Doc Name
PROPOSED DECISION AND FINDINGS OF COMPLIANCE
Permit Index Doc Type
FINDINGS
Media Type
D
Archive
No
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_18_ <br />Probable Hydrologic Consequences <br />of the Twin Pines No. 2 .Mine <br />Twin Pines Coal Company, Inc. provided information on the probable hydrologic <br />consequences of the mine on pages 94 and 95 of the permit application. This <br />information was supplemented by the report written by J.F. Sato and Associates <br />provided by the Small Operators Assistance Program (S.O.A.P). The probable <br />hydrologic consequences of the proposed T•.vin Pines No. 2 Mine are negligible <br />on the scale of the general area. However, the Division has identified <br />several potential impacts to the prevailing hydrologic balance in the permit <br />and adjacent areas. Possibly impacts to the prevailing hydrologic balance <br />within the permit and adjacent area are discussed according to the following <br />format: first, the hydrologic regime; secondly, the uses made of the water <br />resource; thirdly, the probable hydrologic consequences to the water resource; <br />and last, the resolution of the identified problem. <br />A. Ground Water <br />Ground water within the permit and adjacent area is similar to that in the <br />general area in that there are three ground water systems: the Trinidad <br />Sandstone, alluvial aquifers and aquifers within the Vermejo Formation. <br />The Trinidad Sandstone is approximately 600 feet below the Brookside seam <br />which is proposed for mining at the Twin Pines No. 2 Mine. No use is made of <br />this aquifer within the permit and adjacent area. The two strata are <br />separated by many impermeable zones and are not hydrologically connected by <br />faults or fractures. Therefore, the probable impact to the Trinidad Sandstone <br />aquifer is negligible. <br />An alluvial aquifer is found along the flood plain of Oak Creek, one mile <br />north of the permit area. Unconsolidated alluvial materials, consisting of <br />sand, gravel and clay are found along Oak Creek. This alluvium is estimated <br />to be a maximum of 30 feet thick overlying the consolidated bedrock. The <br />water level in the alluvium is in direct contact with the surface water levels <br />and flow of Oak Creek. The alluvium of Oak Creek serves as the source of <br />water for the town of Rockvale's water system, which consists of five hand-dug <br />wells in the alluvium of Oak Creek in Sections 34 and 35, T19S, R70W (see <br />Figure 2). A pipeline system connects these wells and water flows by gravity <br />to the reservoir system west of town. <br />During the permitting process, possible impacts to the Oak Creek alluvial <br />aquifer and the source of water for the Rockvale water system were analyzed. <br />The Division determined that surf ace and ground water flows from the permit <br />area do not contribute to the source of water for the Rockvale system because; <br />1) the wells are upstream of the point where surf ace water from the permit <br />area flows into Oak Creek, and 2) the alluvial wells are updip from the mine <br />since the coal seam to be mined dips to the southeast away from the creek. <br />The only potential impact is where the mine access road crosses over the <br />pipeline which supplies water to Rockvale. Twin Pines Coal Company, Inc., has <br />designed the access road to protect the line from damage by placement of more <br />than three feet of cover over the line. <br />
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