
mineral
Pyrite with Quartz
Iron Sulfide (FeS2) with Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6-6.5 (Pyrite) / 7 (Quartz); Color: Brass-yellow (Pyrite), White/Transparent (Quartz); Luster: Metallic (Pyrite), Vitreous (Quartz); Crystal Structure: Isometric (cubic/pyritohedral), Hexagonal (Quartz); Cleavage: Indistinct; Specific Gravity: 4.9-5.2.
- Hardness
- 6-6
- Color
- Brass-yellow (Pyrite), White/Transparent (Quartz)
- Luster
- Metallic (Pyrite), Vitreous (Quartz)
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Physical properties
Hardness: 6-6.5 (Pyrite) / 7 (Quartz); Color: Brass-yellow (Pyrite), White/Transparent (Quartz); Luster: Metallic (Pyrite), Vitreous (Quartz); Crystal Structure: Isometric (cubic/pyritohedral), Hexagonal (Quartz); Cleavage: Indistinct; Specific Gravity: 4.9-5.2.
Formation & geological history
Formed in hydrothermal veins at a variety of temperatures by the precipitation of sulfide and silicate minerals from hot, mineral-rich fluids. It can also occur as an accessory mineral in igneous, metamorphic, and sedimentary rocks.
Uses & applications
Source of sulfur and sulfuric acid in industry; historical source of sparks for firearms; widely used as a collector specimen and in costume jewelry.
Geological facts
Commonly known as Fool's Gold due to its resemblance to precious metal. Historically used in the 'wheel lock' firearms to ignite gunpowder. It is the most common sulfide mineral found on Earth.
Field identification & locations
Identify by its metallic luster, golden color, and green-black streak (unlike real gold). Commonly found in mines in Peru, Spain, Italy, and the USA. This specimen is a 'cluster' or 'combination' piece featuring Druzy Quartz.
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