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2019-04-24_REPORT - C1980007
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2019-04-24_REPORT - C1980007
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Last modified
1/5/2025 4:56:25 AM
Creation date
4/25/2019 7:48:36 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Report
Doc Date
4/24/2019
Doc Name
Subsidence Monitoring Report
From
Mountain Coal Company, LLC
To
DRMS
Annual Report Year
2018
Permit Index Doc Type
Subsidence Report
Email Name
LDS
Media Type
D
Archive
No
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Fall 2015 Subsidence and Geologic Field Observations <br /> South of Divide and Dry Fork Mining Areas <br /> 5.0 CONCLUSIONS <br /> 1. The conceptual B- and E-seam mining model presented in the Exhibit 60 series of the <br /> mining permit has been verified by annual field observations in the various West Elk Mine <br /> mining areas. With the use of longwall mining methods where the uniform downwarping <br /> of the overburden rocks and unconsolidated material act as laterally constrained plates, <br /> cracks in zones under tensile stress narrow with depth, and close at the neutral surface. <br /> Below the neutral surface, the materials are therefore in compression. This has an <br /> important bearing on the hydrologic consequences of longwall mining. Any groundwater <br /> or surface water in contact with a given subsidence crack is prevented from traveling <br /> downward beyond the neutral surface of the deformed plate. Annual field observations <br /> from 1996 to spring 2018, inclusive, verify this conceptual model in bedrock and surficial <br /> material (colluvium, alluvium, mudflow, and debris flow deposits) where the overburden <br /> is laterally constrained. <br /> 2. Typically, uniform downwarping occurs in association with longwall mining when there <br /> is lateral constraint. Where there are steep slopes and cliffs, there is little to no lateral <br /> support in at least one direction, which causes the associated rocks and unconsolidated <br /> materials to deform like unconstrained beams,plates, or cantilevers as the longwall mining <br /> faces move beneath them. This lack of lateral constraint allows subsidence cracks to <br /> commonly extend completely through sandstones and other brittle units, and groundwater <br /> or surface water present near or within these cracks will likely flow through and exit into <br /> existing surface drainages. The relatively few cliffs and over-steepened slopes in the <br /> Southern Panels Mining Area tend to provide the lateral constraint needed to produce a <br /> more uniform down-warping with fewer significant subsidence cracks observable at the <br /> surface. <br /> 3. To date,there have been no observed or reported water losses associated with the longwall <br /> mining activities. <br /> 831-032.798 Wright Water Engineers, Inc. Page 22 <br /> November 2016 <br />
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