
mineral
Gold bearing Quartz with Sulfides
Auriferous Quartz with Pyrite/Arsenopyrite (Au + SiO2)
AI-generated identification · may be incorrectHardness: 7 (Quartz) to 6 (Pyrite); Color: Rusty brown, grey, yellowish-white with metallic inclusions; Luster: Vitreous to metallic; Crystal Structure: Hexagonal (Quartz), Cubic (Pyrite)
- Hardness
- 7 (Quartz) to 6 (Pyrite)
- Color
- Rusty brown, grey, yellowish-white with metallic inclusions
- Luster
- Vitreous to metallic
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Physical properties
Hardness: 7 (Quartz) to 6 (Pyrite); Color: Rusty brown, grey, yellowish-white with metallic inclusions; Luster: Vitreous to metallic; Crystal Structure: Hexagonal (Quartz), Cubic (Pyrite)
Formation & geological history
Formed in hydrothermal veins where hot, mineral-rich fluids circulate through crustal fractures, often associated with orogenic belts and volcanic activity.
Uses & applications
Primary source for gold extraction in mining; specimen collecting for prospectors and mineral enthusiasts.
Geological facts
The rusty 'gossan' appearance on the surface is caused by the oxidation of iron-bearing sulfide minerals, which often act as a pathfinder for gold deposits.
Field identification & locations
Identify by high density, presence of metallic 'flecks' or sulfides, and heavy iron-oxide staining (rust). Commonly found in historic gold-mining districts.
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