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The water from 69 small streams draining an average area of 1 square mile in the piedmont of South Carolina was sampled at low flow and tested for unusually high content of inorganic chemical constituents. The tests were made to determine whether the unusual amounts of dissolved constituents that had been found in the water of several shallow domestic wells also occurred in the streams and, thus, whether small streams rather than wells could be used for hydrogeochemical prospecting. The water was tested for specific conductance, hardness, pH, and iron and chloride content. Seven of the streams having the highest specific conductance, hardness, and chloride content were given complete water analysis. The results indicate that water from streams draining crystalline rocks of the Carolina slate belt is different in specific conductance and hardness from water in streams draining areas that have a layer of coastal-plain sedimentary rocks overlying the crystalline rocks. No areas were found in which the water had unusually high dissolvedmineral content.

Geochemical prospecting using water from small streams in central South Carolina