
mineral
Pyrite in Quartz
Silicon Dioxide (SiO2) with Iron Sulfide (FeS2)
AI-generated identification · may be incorrectHardness: 7 (Quartz) and 6-6.5 (Pyrite). Color: Colorless to white quartz with metallic brassy-yellow pyrite. Luster: Vitreous to metallic. Crystal Structure: Hexagonal (Quartz) and Isometric/Cubic (Pyrite).
- Hardness
- 7 (Quartz) and 6-6
- Color
- Colorless to white quartz with metallic brassy-yellow pyrite
- Luster
- Vitreous to metallic
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Physical properties
Hardness: 7 (Quartz) and 6-6.5 (Pyrite). Color: Colorless to white quartz with metallic brassy-yellow pyrite. Luster: Vitreous to metallic. Crystal Structure: Hexagonal (Quartz) and Isometric/Cubic (Pyrite).
Formation & geological history
Forms in hydrothermal veins where hot, mineral-rich fluids circulate through fractures in rocks, precipitating quartz and sulfide minerals as they cool. Common in igneous and metamorphic environments.
Uses & applications
Used primarily as decorative specimens for collectors, metaphysical purposes, and sometimes as a minor source of sulfur or iron, though quartz is used in electronics and glass-making.
Geological facts
Pyrite is famously known as Fool's Gold due to its resemblance to precious metal. When found inside quartz, it creates a striking contrast that is highly prized by mineral collectors.
Field identification & locations
Identify by looking for the metallic gold-colored flecks or cubes embedded within a translucent or white hard matrix that cannot be scratched by a steel knife. Common in mining districts worldwide, such as Peru, Spain, and the USA.
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