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Energy Fuels Coal, Inc. <br />Southfield Mine <br />SEMI-ANNUAL SUBSIDENCE MONITORING REPORT <br />(Period: November 1, 1994 -April 30, 1995) <br />Introduction <br />The semi-annual subsidence monitoring report includes a summary comparison of survey <br />monitoring results and tfie predictions for inventoried structures. Additionally, tabulated survey <br />data is attached showing location and orientation of monuments and structures. Cross-sections are <br />attached that graphically represent survey elevation data at the high-resolution monument grid. <br />Discussion <br />1. South Subsidence (High-Resolution) Grid <br />The South Subsidence Grid was surveyed on asemi-annual basis to determine orientation changes <br />of the 23 monuments. Location of the monument grid and the mine layout are shown on Map 17 <br />in the permit application. Summarized survey data for the period of this report are shown on <br />Table 1, Semi-Annual Subsidence Monitoring Data Summary. These data are also shown <br />graphically, in cross-section form, on Figures 1 and 2. From the vertical displacement data <br />plotted on Figure 1, the estimated draw angle is depicted. <br />Comparison of the monitoring data and subsidence predictions show that the maximum surveyed <br />subsidence, 2.30 feet at Monument 15, exceeds the permit prediction of 1.46 feet. Tn addition, <br />the subsidence at adjacent Monuments 13 and 14 also exceeds the maximum expected value. The <br />higher than expected subsidence values are a result of mining a second, wide panel adjacent to <br />the monitored panel and under the above mentioned monuments (shown on Map 17). The <br />increased subsidence due to mining wider panels is explained in the Rocky Mountain <br />Geotechnical report located in Exhibit 23 of the permit application. <br />The survey data show that little or no movement of the monuments occurred during the reporting <br />period. This condition is consistent with preceding monitoring periods. It is likely that the caved <br />area and the overlying strata has wnsolidated and is becoming stabilized <br />The estimated angle of draw, shown on Figure 1, is 28.5 degrees. This compares favorably with <br />the 29 degree maximum angle predicted in the permit application. <br />EFCI conducted visual inspections for surface cracking while performing the field surveys. These <br />inspections concentrate on the areas of the surveyed monuments. Surface cracking occurs <br />between Monuments 11 and 12 on the north-leg of the high-resolution grid. This consists of one <br />crack, approximately 40 feet long and a maximum of 1 inch wide. This crack is approximately 4 <br />years old, and is slowly healing during precipitation events since it occurs in the thick surface <br />colluvium materials. <br />