
mineral
Pyrite and Quartz Agglomerate
Iron Sulfide (FeS2) with Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6-6.5 (Pyrite) and 7 (Quartz); Color: Metallic gold/brass with white/clear translucency; Luster: Metallic and vitreous; Crystal structure: Isometric (cubes) and Trigonal; Cleavage: Indistinct; Specific gravity: 4.9-5.2.
- Hardness
- 6-6
- Color
- Metallic gold/brass with white/clear translucency
- Luster
- Metallic and vitreous
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Physical properties
Hardness: 6-6.5 (Pyrite) and 7 (Quartz); Color: Metallic gold/brass with white/clear translucency; Luster: Metallic and vitreous; Crystal structure: Isometric (cubes) and Trigonal; Cleavage: Indistinct; Specific gravity: 4.9-5.2.
Formation & geological history
Forms in hydrothermal veins, as an accessory mineral in igneous rocks, and in sedimentary environments through precipitation in low-oxygen, sulfur-rich conditions.
Uses & applications
Primarily collected as mineral specimens; Pyrite is historically used for sulfur dioxide production and as a gemstone (marcasite jewelry), while Quartz is used in electronics and glass.
Geological facts
Commonly known as Fool's Gold due to its resemblance to precious metal. Pyrite can actually spark when struck against steel, which led to its name derived from the Greek word for fire.
Field identification & locations
Identify by its metallic luster, greenish-black streak (on a streak plate), and brittle nature compared to malleable gold. Found globally in mining districts.
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Epidote
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Granite (Phaneritic intrusive igneous rock)
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