Rock Identifier
Auriferous Quartz or Pyritic Ore (Iron Pyrite (FeS2) or Native Gold (Au) in Matrix) — mineral
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
Identified More mineral

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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.