
mineral
Pyrite
Iron Disulfide (FeS2)
Hardness: 6-6.5 on Mohs scale; Color: Pale brass-yellow to golden; Luster: Metallic; Crystal Structure: Isometric (cubic, octahedral, or pyritohedral); Cleavage: Indistinct; Specific Gravity: 4.88-5.10
- Hardness
- 6-6
- Color
- Pale brass-yellow to golden
- Luster
- Metallic
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Pale brass-yellow to golden; Luster: Metallic; Crystal Structure: Isometric (cubic, octahedral, or pyritohedral); Cleavage: Indistinct; Specific Gravity: 4.88-5.10
Formation & geological history
Forms in diverse geological environments, including high-temperature hydrothermal veins, as an accessory mineral in igneous rocks, and in sedimentary rocks through biological or chemical precipitation in oxygen-poor environments.
Uses & applications
Used industrially as a source of sulfuric acid and sulfur, occasionally in low-cost jewelry (often marketed as 'marcasite'), and widely collected by mineral enthusiasts for its aesthetic cubic crystals.
Geological facts
Commonly known as 'Fool's Gold' due to its resemblance to real gold; however, pyrite is harder and leaves a greenish-black streak, whereas gold is soft and leaves a yellow streak. It can create sparks when struck against steel.
Field identification & locations
Identify in the field by its distinct metallic luster, hardness (it cannot be scratched by a copper coin), and its brittle-crushing nature unlike malleable gold. Common locations include Peru, Spain (Rio Tinto), and Italy.
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