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Marcasite (White Iron Pyrite) is often mistakenly confused with pyrite, but marcasite is lighter and more brittle. Specimens of marcasite often crumble and break up due to the unstable crystal structure, and it is this crystal structure that is the main difference between marcasite and pyrite. Though marcasite has the same chemical formula as pyrite, it crystallizes in a different crystal system, thereby making it a separate mineral. In jewelry, pyrite used as a gem is improperly termed "marcasite". This is wholly incorrect, as marcasite is never used as a gem.

FeS2 - Iron Sulfide
Class:
Orthohombic
Tin-white, bronze-yellow, tarnishing iridescent.
Grayish to brownish black
Metallic
Opaque
4.9
6 - 6.5
Good
Uneven
Tabular, pyramidal and prismatic crystals often twinned into the form of cockscomb like aggregates, stalactitic, botryoidal and massive.
Non-fluorescent
Frequency:
Abundant
Origin:
It originates at low temperatures in very acidic environments, either in sedimentary or in hydrothermal deposits, associated with pyrite, pyrrhotite, galena, sphalerite, fluorite, dolomite & calcite.
Occurence:
Essen, Germany; Joplin, MIssouri, USA; Galena & Sparta, Illinois, USA; Champagne, France; Vintirov, Czech Republic; Reocin Santander, Spain.
Application:
Production of sulfuric acid, mineral specimen

 

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