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<br />o <br />t\:l <br />...... <br />~\.) <br /> <br />10.60 <br /> <br /> <br />9.00 <br /> <br />7.60 <br /> <br />6.00 <br /> <br />4.60 <br /> <br />3.00 <br /> <br />1.60 <br /> <br />1.82 3.33 4.85 <br /> <br />186 9.40 10.91 <br /> <br />0.'l0 <br />'VO "." ".<6 '6." ,....., <br /> <br />'l.oo <br /> <br />T <br /> <br />6.? <br />.- <br />a.. w <br />C1l <br />o <br />cr <br /> <br />o 1000 ft <br />1....______1 <br /> <br />Figure 6. Results of an electrical resistivity survey done using a dipole-dipole <br />electrode array with a dipole length of 30 feet and n=8. The area within the 35 <br />ohm-meter contour, which is considered to be the alluvial aquifer saturated with <br />a mixture of thermal water and normal ground water, is shown as shaded. <br /> <br />9 <br />