FeS
Cubic -- diploidal
Environment
Ubiquitous; in all classes of rocks and all types of veins.
Crystal description
Often crystallized, most frequently in striated cubes, less commonly in octahedrons. Massive pyrite is common.
Physical properties
Light yellow.
Luster
metallic;
hardness
6-6Ɖ;
specific gravity
5.0;
streak
powdery greenish black;
fracture
conchoidal;
cleavage
none. Brittle.
Composition
Iron sulfide (46.6% Fe, 53.4% S).
Tests
Fuses easily, becoming magnetic and giving off sulfur dioxide (SO
2
) fumes. Insoluble in hydrochloric acid, but a fine powder will dissolve in concentrated nitric acid (HNO
3
).
Distinguishing characteristics
The tarnished sulfide might be confused with chalcopyrite, but its great hardness is distinctive. It is slightly yellower and more slowly soluble in nitric acid than marcasite, giving a clear solution. It is harder than gold, and very brittle.
Occurrence
Any weathered rock formation that appears rust-stained probably contains--or contained--pyrite, a frequent associate of all sorts of metal ores. In addition, it forms concretionary masses in sedimentary rocks, which then frequently alter to very compact limonite balls. Golden discs called "pyrite dollars" are found in an Illinois coal formation, and more spherical concretions with brown oxidized skins are common in clays, slates, and other metamorphic rocks. Daisylike golden crystal disks with coarse cubic "petal" rims were found during the Dallas-Fort Worth airport construction. So often mistaken for gold it is popularly known as "fool's gold." Fine specimens have been found throughout the world. Particularly notable in the past were the large well-formed crystals from Leadville, Colorado, and well-developed crystal groups from Park City, Utah. Misshapen octahedral crystals containing 0.2 percent arsenic were found at French Creek, Pennsylvania. "Cathedral" pyrite was a name given to the large cubes with Gothic arch growth patterns on their faces. Many-faced complex and perfect crystals come from Rio Marina on the island of Elba, Italy. Quiruvilca and Cerro de Pasco, both in Peru, now yield outstanding octahedral crystals and pyritohedral groups. Many Mexican occurrences have been reported. Highly modified crystals in fine clusters are typical of Oruro and Colavi, Bolivia. Falun, Sweden, yielded a pyrite rich in cobalt. Fantastic groups of sharp cubes are broken from a limestone in Spain and reconstructed into startling staircases with cubes of up to 5 cm or more.
Remarks
Pyrite was once important as a source of sulfur for the manufacture of sulfuric acid, and could be again. Invisible specks of gold between the grains frequently provide value to seemingly worthless but cyanide-leachable deposits, so it may be an important ore of gold.