“…Conditioned by the high rainwater, high temperature, and by the action of the acid decay of the Amazon rainforest, which brings the pH of the groundwater to 4.5-5.5, the chemical weathering is quite intense, and the rocks are decomposed below the water table. Some of the solubilized components, like manganese, iron, aluminum, and silicon, reprecipitate soon after the rock decomposition, forming supergene oxides and hydroxides of manganese (cryptomelane, lithiophorite and pyrolusite), of iron (limonite, goethite and hematite), aluminum (gibbsite), and silica (Scarpelli 2022). Some of the dissolved elements, such as potassium, cobalt and arsenic, have chemical affinities with manganese and iron, and stay in the crystalline structure of some of the supergene manganese and iron minerals, not representing a health problem for the mine workers and for the inhabitants of Serra do Navio.…”