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TABLE G-85 <br /> AVERAGEI <br /> AVERAGE CONDUCTIVITY <br /> LOCATION WATER LEVEL ELEVATION AVERAGE pHl @250°C <br /> <br /> D-1 108.2 6322.8 8.6 4050 <br /> D-2 108.2 6323.3 <br /> D-3 79.5 6581.6 <br /> E-1 72.3 6359.1 8.2 952 <br /> E-2 73.4 6360.4 <br /> E-3 102.3 6560.4 <br /> F-1 22.6 6408.7 8.6 556 <br /> A-1 10.0 6488.0 7.5 595 <br /> A-2 17.6 6494.5 <br /> A-3 5.8 6524.6 <br /> A-4 6.1 6527.4 <br />• A-5 14.5 6533.0 <br /> A-6 23.6 6502.9 <br /> A-72 29.3 6520.0 <br /> A-82 37.7 6419.9 <br /> A-9 13.8 6426.9 7.5 248 <br /> A-10 13.2 6424.6 <br /> A-11 17.8 6415.7 7.1 529 <br /> A-122 15.5 6416.7 <br /> S-1 16.8 6452.5 <br /> R-1 26.7 6411.4 5.0 10533 <br /> R-2 None <br /> R-3 21.2 6406.1 6.4 6981 <br /> R-4 40.8 6412.5 <br /> R-5 None <br /> R-6 28.3 6351.6 6.4 9440 <br /> P-1 10.1 6316.3 7.3 1998 <br /> P-2 9.2 6316.4 7.3 1660 <br />• P-3 11.3 6317.5 7.3 1436 <br /> P.-4 ~2:3~ 6322.2 <br />lAlluvial and coal seam. points only sampled once. <br />2TO calculate the average water level, the depth of the piezometer <br />was used when no water was found. <br />