Fluorite is a calcium fluoride mineral, with the chemical formula CaF₂.
Fluorite occurs worldwide and is found in veins associated with hydrothermal deposits, as well as in sedimentary rocks.
Fluorite is primarily used in the production of hydrofluoric acid, which is a key component in the manufacture of aluminum and uranium fuel, as well as in the production of fluorine-based chemicals.
Fluorite was known in antiquity, and its name comes from the Latin word "fluere", meaning "to flow", due to its use as a flux in steelmaking.
Fluorite has a hardness of 4 on the Mohs scale and typically occurs in cubic crystals. It comes in a variety of colors, including purple, blue, green, yellow, and colorless.
Fluorite forms in low- to medium-temperature hydrothermal veins, often filling cavities and fractures in rocks.
Fluorite is known for its remarkable fluorescence, glowing under ultraviolet light in various colors depending on the impurity content. It has a vitreous luster and is transparent to translucent.
Fluorite is classified as a halide mineral, with a cubic crystal system and a chemical composition of calcium fluoride (CaF₂).
Fluorite is often used in the production of colored glass and enamels, and is sometimes used as a gemstone in jewelry. It is also a key mineral for scientists studying fluorescence.