In Tamatsukuri Hot-Springs, the chloride and sulfate content and water temperatures of well waters and the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from various parts of the mineral spring districts. For the values which were determined with samples collected from the thermal spring districts and its neighbourhood, no difference was recognized. This result is quite different from the results given in the previous reports of the present author. But this fact may be explaned as the effects of the sea warter, and the further study is being continued.