The Panyam volcanic province is a plateau covering a superficial area of about 1200 km 2 , dotted by a number of dormant volcanoes forming prominent landmarks above the host continental gneiss-migmatite-granite rocks and stretching for about 12 km. The volcanism is basaltic, characterized by alkaline-calc-alkaline compositions. Large population of people live and depend on the volcanic environment for potable water and agriculture, most of whom display various forms of health problems ranging from dental caries, goitre, podoconiosis, etc. This study therefore seeks to evaluate the concentration levels of potentially harmful elements (PHEs) in the various components of the volcanic environment and their relationship with the inherent human health problems in the area. Volcanic soils and underground waters (springs/boreholes waters) were collected from within the volcanic province for the analysis of major cations and anions. Samples of the volcanic soils were analyzed for the following heavy elements; Be, Co, Cr, Cu, As, Cd, Pb, Sb, Se, V, and Zn. The significantly lower La/Ce ratios (0.30-0.57) in the volcanic soils attest to the moderate to slightly severe intensity of weathering the parent basaltic rock was subjected to. The waters are predominantly (80 %) of Ca-Mg-HCO 3 type with the remaining 20 % of Na-K-HCO 3 type suggesting a control by water-rock alteration process from the host granitic basement and the overlying basaltic rocks. The fluoride content in all the water sources is positively correlated with the contents of Mg 2? , Na ? , and K ? suggesting a similar source and geochemical process. Tooth decay, a common tooth disease conditions in the volcanic province, could be linked to the low F content in the waters.