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2021-02-05_PERMIT FILE - C1980007A (5)
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2021-02-05_PERMIT FILE - C1980007A (5)
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Last modified
10/6/2022 8:32:15 PM
Creation date
2/23/2021 11:01:07 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1980007A
IBM Index Class Name
Permit File
Doc Date
2/5/2021
Doc Name
SUBSIDENCE EVALUATION
Section_Exhibit Name
Exhibit 60E Subsidence Evaluation for the South of Divide and Dry Fork Mining Areas
Media Type
D
Archive
Yes
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Subsidence Evaluation for the <br /> Exhibit 60E Southern Panels, Apache Rocks West, & Sunset Trail Mining Areas Page 29 <br /> 10.0 POTENTIAL IMPACTS OF SUBSIDENCE AND MINE-INDUCED <br /> SEISMIC ACTIVITY ON LANDSLIDES AND ROCKFALLS <br /> 10.1 Landslides <br /> The landslides listed below are all naturally occurring features, which become less stable, or <br /> become unstable and slide, during periods of increased precipitation. A review of aerial <br /> photographs of the Apache Rocks and South of Divide mining areas, which were taken in 1963 <br /> and 2004, show that the slides listed below appeared to be more stable in 1963 than they are now. <br /> Mr. C. Richard Dunrud (retired U.S. Geological Survey coal mine subsidence expert and author <br /> of USGS Map C-115) observed that many of the existing landslides during periods of high <br /> precipitation were less stable, or became unstable and moved in the mid-1980s and mid-1990s. <br /> Landslides were identified in the Dry Fork mining area as part of the Final Environmental Impact <br /> Statement (2005). Map 1 is a composite showing the landslides in the Southern Panels mining <br /> area. <br /> The landslides in the southeast side of West Flatiron and on the west side of Deep Creek in the <br /> Apache Rocks mining area showed no visual effects when longwall mining occurred beneath the <br /> areas. It therefore seems apparent that wet seasons affect landslides more than does longwall <br /> mining. During very wet periods, however, landslides that are already unstable may locally be <br /> triggered by mine subsidence. <br /> A total of twelve landslides, landslide areas, or landslide and rockfall areas, have been mapped in <br /> the Apache Rocks West and Southern Panels mining areas during field mapping with the U.S. <br /> Geological Survey (USGS) in the 1980s and also during the annual subsidence observations in <br /> these areas. <br /> 1. Apache Rocks West mining area: <br /> a. Landslide located just north of Minnesota Reservoir in SW'/4 of Section 29. Mining of <br /> the B-seam longwall panels 1312, 1313, and B 13-A did not have any observable effect <br /> on the landslide. <br /> b. Landslide area located above mined longwall panels E14 and E15 in NW'/4 of Section <br /> 26. These landslides appeared to be unaffected by longwall mining beneath them. <br /> c. Landslide area located on the west side of Deep Creek, located above the southeastern <br /> part of mined B-seam longwall panel 17 in the NW'/4 of Section 35. This landslide also <br /> appeared to be unaffected by mining below when observed in July 2003. <br /> 2. Southern Panels mining area(Map 1): <br /> a. An extensive landslide is located south of Minnesota Reservoir north of the projected <br /> E-seam longwall panel E9, in the N'/2 of Section 32, Township 13 South, Range 90 <br /> West (Dunrud 1989). Overburden depth to the E-seam ranges from 500 to 600 feet. <br /> The average slope of the slide is roughly 20 percent. The landslide contains more <br /> cracks and scarps in the upper part and more depressions and bulges in the lower part <br /> 831-032.912 Wright Water Engineers, Inc. <br /> December 2020 <br />
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