
mineral
Quartz with Pyrite
Silicon Dioxide (SiO2) with Iron Sulfide (FeS2)
Hardness: 7 (Quartz) and 6-6.5 (Pyrite). Color: Clear/Grey host with metallic brassy-yellow flecks. Luster: Vitreous (Quartz) to Metallic (Pyrite). Crystal structure: Trigonal/Hexagonal and Cubic.
- Hardness
- 7 (Quartz) and 6-6
- Color
- Clear/Grey host with metallic brassy-yellow flecks
- Luster
- Vitreous (Quartz) to Metallic (Pyrite)
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Physical properties
Hardness: 7 (Quartz) and 6-6.5 (Pyrite). Color: Clear/Grey host with metallic brassy-yellow flecks. Luster: Vitreous (Quartz) to Metallic (Pyrite). Crystal structure: Trigonal/Hexagonal and Cubic.
Formation & geological history
Formed in hydrothermal veins through circulating hot, mineral-rich fluids in the earth's crust. It is often found in metamorphic or igneous environments across many geological ages, particularly associated with volcanic activity.
Uses & applications
Quartz is used in electronics (oscillators), glass making, and abrasives. Pyrite is an ore of sulfur and a collector's specimen. Together they are valued for mineral collecting and ornamental decoration.
Geological facts
Pyrite is famously known as 'Fool's Gold' because its color and metallic luster often tricked prospectors. Quartz is the second most abundant mineral in the Earth's continental crust.
Field identification & locations
Identify by scratching glass with the quartz (hardness check) and observing the metallic, cubic structure of the pyrite. Found in mountain ranges, mines, and riverbeds globally. Collectors look for sharp metallic cubes nestled in clear crystal faces.
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