Early occurrences of realgar as a red paint pigment are known for works of art from China, India, Central Asia, and Egypt. It was used in European fine-art painting during the Renaissance era, a use which died out by the 18th century. It was also used as medicine. Other traditional uses include manufacturing lead shot, printing, and dyeing calico cloth. It was used to poison rats in medieval Spain and in 16th century England. Occurrence Realgar most commonly occurs as a low-temperature hydrothermal vein mineral associated with other arsenic and antimony minerals. It also occurs as volcanic sublimations and in hot spring deposits. It occurs in association with orpiment, arsenolite, calcite and barite. It is found with lead, silver and gold ores in Hungary, Bohemia and Saxony. In the US it occurs notably in Mercur, Utah; Manhattan, Nevada; and in the geyser deposits of Yellowstone National Park. After a long period of exposure to light, realgar changes form to a yellow powder known as pararealgar (β-). It was once thought that this powder was the yellow sulfide orpiment, but is a distinct chemical compound. Gallery See also Classification of minerals List of inorganic pigments List of minerals References Further reading The Merck Index: An Encyclopedia of Chemicals, Drugs, and Biologicals. 11th Edition. Ed. Susan Budavari. Merck & Co., Inc., N.J., U.S.A. 1989. William Mesny. Mesny’s Chinese Miscellany. A Text Book of Notes on China and the Chinese. Shanghai. Vol. III, (1899), p. 251; Vol. IV, (1905), pp. 425–426. American Mineralogist Vol 80, pp 400–403, 1995 American Mineralogist Vol 20, pp 1266–1274, 1992 External links Mindat.org: Pararealgar Arsenic minerals Sulfide minerals Alchemical substances Monoclinic minerals Minerals in space group 14 Inorganic pigments