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Fall 2014 Subsidence and Geologic Field Observations <br />South of Divide and Dry Fork Mining Areas <br />during the spring 2014 field visit. Figure 4 shows the same location from approximately the same <br />vantage point as observed during the fall 2014 field visit. Note the considerable healing and <br />sealing of these cracks due to weathering. <br />Figure 3. Spring 2014 image looking south /southeast at several small differential settlement cracks exacerbated by <br />subsidence along the eastern portion of the E4 -1/2/3 MDW pad with the greatest vertical fill depth. <br />Figure 4. Fall 2014 image looking south /southeast at the same area shown in Figure 3. <br />evidence of the cracks due to weathering. <br />3.6 Traverse F -F' <br />Note the subdued visual <br />This traverse originates along the south side of the Dry Fork Road and travels southeastward <br />parallel to the Dry Fork for approximately 4,000 feet and then continues southward up Poison <br />Gulch (next significant drainage east of Deer Creek). This traverse crosses mined portions of E- <br />seam Longwall Panels E3 and E4 as well as unmined portions of E -seam Longwall Panels E5 and <br />831 - 032.796 Wright Water Engineers, Inc. Page 10 <br />March 2015 <br />