Barite

Definition and stakes

Portrait of Frederic Brewster Loomis Frederic Brewster Loomis,  Field Book of Common Rocks and Minerals

“ Barite is a secondary mineral of aqueous origin, which has been deposited in veins and cavities in igneous, metamorphic, or sometimes sedimentary rocks. It is most likely to occur in veins in igneous or metamorphic rocks, the barium having been dissolved from certain feldspars and micas by percolating water, and then redeposited in the fissures, as the water came into them. If in sedimentary rocks, the barite veins are usually in limestones. Barite is quite likely to be a gangue mineral for the ores of lead. ”
Source: Gutenberg

The New International Encyclopædia…

“ Barite, or barytes as it is called commercially, is used as a substitute for or an adulterant of white lead in the manufacture of white pigments; for this purpose it must be free from iron, and therefore its preparation for market consists not only in grinding, but in some cases may include treatment with sulphuric acid to remove the stains. The main supply of barite is obtained from Missouri, North Carolina, Virginia, and Tennessee. It is cheaper than white lead, and does not turn yellow on exposure to the air. ”
Source: Wikisource

C. K. Leith,  The Economic Aspect of Geology

“ The fact that barite is a characteristic mineral of many igneous veins, and the fact that in this same general region it is found in the Kentucky-Illinois fluorspar deposits,—where a magmatic source is generally accepted,—together with doubts as to the theoretical efficacy of meteoric waters to transport the minerals found in the barite deposits, have led certain writers to ascribe to these barite deposits a magmatic origin. The magmatic theory has not been disproved ”
Source: Gutenberg

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