
mineral
Quartz with Pyrite inclusions
Silicon Dioxide (SiO2) with Iron Sulfide (FeS2)
AI-generated identification · may be incorrectHardness: 7 (Quartz) / 6-6.5 (Pyrite). Color: Milky to translucent white with metallic brassy-gold spots. Luster: Vitreous to greasy on quartz, metallic on pyrite. Crystal structure: Hexagonal/Trigonal. Cleavage: None (conchoidal fracture).
- Hardness
- 7 (Quartz) / 6-6
- Color
- Milky to translucent white with metallic brassy-gold spots
- Luster
- Vitreous to greasy on quartz, metallic on pyrite
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Physical properties
Hardness: 7 (Quartz) / 6-6.5 (Pyrite). Color: Milky to translucent white with metallic brassy-gold spots. Luster: Vitreous to greasy on quartz, metallic on pyrite. Crystal structure: Hexagonal/Trigonal. Cleavage: None (conchoidal fracture).
Formation & geological history
Formed through hydrothermal processes where mineral-rich hot water circulates through crustal fractures. Pyrite crystals often grow alongside or inside the quartz as the solution cools and crystallizes.
Uses & applications
Primarily used for geological collecting and as a indicator mineral for gold prospecting. Pure quartz is used in glassmaking and electronics; pyrite is used for sulfuric acid production but is mostly a specimen mineral here.
Geological facts
Pyrite is known as 'Fool\'s Gold' because its color and metallic luster frequently lead novice prospectors to mistake it for genuine gold. Quartz is the second most abundant mineral in Earth\'s continental crust.
Field identification & locations
Identify in the field by the quartz\'s ability to scratch glass and the pyrite\'s metallic, cubic structure. Found commonly in mountainous regions and near mining districts or quartz veins.
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