Abstract
An evaluation of the mercury concentration in soils of six Colorado geothermal areas is completed utilizing regression analysis. Regression analysis incorporated the secondary effects of pH and the organic carbon, iron, and manganese concentrations on mercury in soils. The technique is used to evaluate a geothermal anomaly at Glenwood Springs, Colorado. The results indicate that secondary influences on mercury in soils of geothermal areas may be of importance in evaluating areas of anomalous mercury leakage.
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