
mineral
Auriferous Quartz or Pyritic Ore
Iron Pyrite (FeS2) or Native Gold (Au) in Matrix
Hardness: 6-6.5 (Pyrite) or 2.5-3 (Gold); Color: Brassy yellow metallic inclusion in grey/blue host rock; Luster: Metallic; Crystal Structure: Isometric; Cleavage: Indistinct; Specific Gravity: Approx 5.0
- Hardness
- 6-6
- Color
- Brassy yellow metallic inclusion in grey/blue host rock
- Luster
- Metallic
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Physical properties
Hardness: 6-6.5 (Pyrite) or 2.5-3 (Gold); Color: Brassy yellow metallic inclusion in grey/blue host rock; Luster: Metallic; Crystal Structure: Isometric; Cleavage: Indistinct; Specific Gravity: Approx 5.0
Formation & geological history
Formed in hydrothermal veins where mineral-enriched hot fluids circulate through fractures in the Earth's crust, often associated with metamorphic or igneous activity. Commonly found in quartz veins and greenstone belts.
Uses & applications
Primary source of gold if the inclusions are native gold; used as iron ore and for sulfuric acid production if pyrite. High interest for mineral collectors and prospectors.
Geological facts
Often called 'Fool's Gold' because pyrite is commonly mistaken for real gold. Some pyrite specimens contain small amounts of actual gold hidden within the crystal structure.
Field identification & locations
Identify by checking for streak color (pyrite has a greenish-black streak, gold has a golden-yellow streak) and checking if it is brittle (pyrite will shatter, gold will flatten). Found in active gold mining regions globally.
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