
mineral
Pyrite (locally known as Fool's Gold)
Iron Sulfide (FeS2)
AI-generated identification · may be incorrectHardness: 6–6.5 (Mohs), Color: Pale brass-yellow, Luster: Metallic, Crystal system: Isometric/Cubic, Cleavage: Indistinct, Specific Gravity: 4.9–5.2
- Hardness
- 6–6
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Physical properties
Hardness: 6–6.5 (Mohs), Color: Pale brass-yellow, Luster: Metallic, Crystal system: Isometric/Cubic, Cleavage: Indistinct, Specific Gravity: 4.9–5.2
Formation & geological history
Formed in both igneous and sedimentary environments via hydrothermal activity or sulfur reduction. Often found in quartz veins or associated with coal beds and metamorphic rocks.
Uses & applications
Historical source of sulfur and sulfuric acid. Used as an ornamental stone in 'marcasite' jewelry and as a semiconductor in early radio receivers.
Geological facts
Its nickname 'Fool's Gold' comes from its resemblance to real gold, though it is much harder and more brittle. Unlike gold, pyrite can create sparks when struck against steel.
Field identification & locations
Identify by its hardness (cannot be scratched by a copper penny) and its blackish-green streak on a porcelain plate. Common worldwide, especially in Spain, Russia, and the USA.
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