
mineral
Pyrite
Iron Sulfide (FeS2)
Hardness: 6-6.5 on Mohs scale; Color: Pale brass-yellow to golden; 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 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 (often cubic, pyritohedral, or octahedral); Cleavage: Indistinct; Specific Gravity: 4.9-5.2
Formation & geological history
Formed in hydrothermal veins, as an accessory mineral in igneous rocks, by contact metamorphism, and in sedimentary rocks like shale and coal. It forms in oxygen-deficient environments.
Uses & applications
Primarily used as an ore for sulfur and sulfuric acid. It is popular as a collector's specimen and used in costume jewelry (marcasite jewelry). Historically used to create sparks for early firearms.
Geological facts
Commonly known as 'Fool's Gold' because its color and high specific gravity lead many to mistake it for gold. Unlike real gold, it is brittle and will shatter if struck rather than flatten.
Field identification & locations
Identify by its brittle nature, greenish-black streak (gold has a yellow streak), and cubic crystal habits. Found worldwide, with notable deposits in Peru, Spain, and the USA.
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Mineral/Rock
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mineral