Images
  
  Formula: Cu3AsS4
  
  Sulpharsenate of copper, 
  paramorph 
  of luzonite
  
  Crystal System: Orthorhombic
  
  Specific gravity: 4.4 to 4.5 measured,  4.40 calculated
  
  Hardness: 3½
  
  Streak: Black
  
  Colour: Steel grey to iron black
  
  Solubility: Slightly soluble in nitric acid
  
  Common impurities: Sb,Fe,Pb,Zn,Ag,Ge 
  
  Environments:
  Enargite is a comparatively rare mineral, found in vein and replacement deposits formed at moderate 
  temperatures 
  associated with pyrite, 
  sphalerite, 
  bornite, 
  galena, 
  tetrahedrite-tennantite, 
  covellite, chalcocite, 
  baryte and quartz  
  (Mindat, HOM).
  
  Localities
  
  At the Pingüino deposit, Tres Cerros, Deseado Department, Santa Cruz Province, Argentina, minor late grains 
  (<50 microns in size) of enargite are present in the cleavage planes of 
  galena or as irregular masses related to 
  freibergite 
  (CM 49.931-946).
  
 
  At Lahóca Hill, Recsk, Pétervására District, Heves County, Hungary, enargite and 
  luzonite occur together in the 
  metasomatised ore bodies 
  (AM 83.365-372).
  
  Enargite from Lahóca Hill - Image
  
  The type locality is the San Francisco vein, Morococha District, Yauli Province, Junín, Peru.
  
  Enargite from the San Francisco vein - 
  Image
  
  
  At the Gregory mine, Ashover, Derbyshire, England, UK, enargite has been found with 
  calcite 
  (RES p103).
  
  At the Ladywash mine, Eyam, Derbyshire Dales District, Derbyshire, England, UK, enargite occurs as metallic 
  grey-black crystals up to about 0.75 mm on edge, with chalcopyrite, 
  galena, pyrite and 
  sphalerite on a fluorite 
  specimen from the workings on Hucklow Edge Vein. The enargite occurs as a late-stage 
  primary phase in low-temperature 
  fluorite-dominated hydrothermal vein mineralisation 
  (JRS 22.6-10).
  
  At Tintic Mining District, Juab County, Utah, USA, enargite generally occurs as metallic masses in 
  quartz matrix; it has also been found as single crystals and crystal groups 
  in pockets of quartz crystals at many of the mines in the district. 
  
  The enargite occurs mainly in coarsely crystalline aggregates of iron-black colour and excellent prismatic 
  cleavage. Some of the individual grains may be 2 or 3 inches in length. Good but very small crystals were seen on 
  quartz in vugs in ore from the Eureka Hill mine. Enargite is 
  associated with baryte and 
  jasperoid, and much of it contains small grains of 
  pyrite and chalcopyrite. Good 
  crystals of enargite, up to 2.5 cm and resting on quartz, have been 
  found at the Tintic Standard mine. On both the upper and lower dumps at the North Star mine, enargite 
  crystals to about 0.5 mm occur on a quartz and 
  baryte matrix associated with 
  azurite, chrysocolla, 
  jarosite, kettnerite, 
  malachite, mixite, 
  pyrite, tetrahedrite and 
  tyrolite 
  (MinRec 55.2.198-201).
  
  Enargite from Tintic - Image
  
  Alteration
  
enargite and pyrite to 
  Fe-tennantite, chalcopyrite 
  and sulphur
  
  4Cu3AsS4 + 4FeS2 → Cu10Fe2As4S13 
  + 2CuFeS2 
  + 7/2S2
  
  (CM 28.725-738)
  
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