
mineral
Pyrite on Quartz matrix
Iron Disulfide (FeS2) on Silicon Dioxide (SiO2)
Hardness: 6-6.5 (Pyrite), 7 (Quartz); Color: Brass-yellow metallic Pyrite on milky white Quartz; Luster: Metallic (Pyrite)/Vitreous (Quartz); Crystal Structure: Isometric (Pyrite cubes/pyritohedrons) and Hexagonal (Quartz); Cleavage: Indistinct; Specific Gravity: 4.9-5.2.
- Hardness
- 6-6
- Color
- Brass-yellow metallic Pyrite on milky white Quartz
- Luster
- Metallic (Pyrite)/Vitreous (Quartz)
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Physical properties
Hardness: 6-6.5 (Pyrite), 7 (Quartz); Color: Brass-yellow metallic Pyrite on milky white Quartz; Luster: Metallic (Pyrite)/Vitreous (Quartz); Crystal Structure: Isometric (Pyrite cubes/pyritohedrons) and Hexagonal (Quartz); Cleavage: Indistinct; Specific Gravity: 4.9-5.2.
Formation & geological history
Formed in hydrothermal veins through the cooling of mineral-rich hot fluids or as a secondary mineral in sedimentary and metamorphic environments. These minerals can range in age from millions to billions of years depending on the host rock formation.
Uses & applications
Primarily used as decorative display specimens for collectors and in jewelry (as 'marcasite'). Pyrite is also a minor ore of sulfur and was historically used to create sparks for firearms.
Geological facts
Pyrite is famously known as 'Fool's Gold' because its metallic luster and brassy hue often led novice prospectors to mistake it for real gold. Unlike gold, it is brittle and will shatter rather than flatten when struck.
Field identification & locations
Identify in the field by its brassy color, cubic crystal habit, and blackish-green streak on a porcelain plate. It is found globally, with significant deposits in Spain, Peru, and the USA (Colorado/Arizona). Collectors look for well-defined crystal faces.
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