
mineral
Pyrite
Iron Sulfide (FeS2)
AI-generated identification · may be incorrectHardness: 6-6.5 on Mohs scale; Color: Pale brass-yellow to tarnished brown; Luster: Metallic; Crystal Structure: Isometric (often cubic, pyritohedral, or octahedral); Cleavage: Indistinct; Specific Gravity: 4.9-5.2.
- Hardness
- 6-6
- Color
- Pale brass-yellow to tarnished brown
- Luster
- Metallic
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Pale brass-yellow to tarnished brown; Luster: Metallic; Crystal Structure: Isometric (often cubic, pyritohedral, or octahedral); Cleavage: Indistinct; Specific Gravity: 4.9-5.2.
Formation & geological history
Formed in high and low-temperature hydrothermal veins, by magmatic segregation, in metamorphic rocks, and as an authigenic mineral in sedimentary rocks. Can be found in geological formations of all ages.
Uses & applications
Major ore for sulfur and sulfuric acid production; historically used in ignition for firearms; used in jewelry (often marketed as 'marcasite') and as popular collector specimens.
Geological facts
Commonly known as 'Fool's Gold' because its color and high density resemble gold. Unlike gold, it is brittle and leaves a greenish-black streak on a streak plate. It can spark when struck with steel.
Field identification & locations
Identify by its cubic shape, metallic luster, and hardness (it cannot be scratched by a copper penny or knife). Commonly found in Spain (Navajún), Italy, and Peru. Watch for 'pyrite disease' where specimens decay in high humidity.
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