
mineral
Auriferous Quartz with Pyrite
Gold-bearing Quartz (SiO2 + FeS2 + Au)
Hardness: 6-7 (quartz) and 6-6.5 (pyrite); Color: White, grey, rusty brown (limonite) with metallic gold/brass yellow flecks; Luster: Vitreous to metallic; Crystal structure: Trigonal/Isometric; Specific Gravity: 2.65-5.0
- Hardness
- 6-7 (quartz) and 6-6
- Luster
- Vitreous to metallic
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Physical properties
Hardness: 6-7 (quartz) and 6-6.5 (pyrite); Color: White, grey, rusty brown (limonite) with metallic gold/brass yellow flecks; Luster: Vitreous to metallic; Crystal structure: Trigonal/Isometric; Specific Gravity: 2.65-5.0
Formation & geological history
Formed in hydrothermal veins where hot, mineral-rich fluids circulate through crustal fractures. Often associated with volcanic activity or metamorphic belts from various geological ages, frequently Ore Archean to Cenozoic.
Uses & applications
Primary source for industrial gold mining, jewelry production, and high-value mineral specimen collecting.
Geological facts
This specimen shows significant iron oxidation (rusting), which is a classic indicator for prospectors that gold-bearing sulfides like pyrite have decomposed, potentially leaving free gold behind.
Field identification & locations
Identify by looking for quartz veins with ‘gossan’ (rusty staining), heavy weight, and cubic pyrite crystals or metallic gold inclusions. Commonly found in California (Mother Lode), Alaska, and Australia.
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