
mineral
Yellow Quartz (Citrine Quartz variety / Ferruginous Quartz)
Silicon Dioxide (SiO2) with iron inclusions
Hardness: 7 on the Mohs scale; Color: Translucent yellow to honey-orange; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on the Mohs scale
- Color
- Translucent yellow to honey-orange
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on the Mohs scale; Color: Translucent yellow to honey-orange; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or as a secondary mineral in sedimentary deposits. The yellow coloration is typically the result of iron impurities or natural irradiation of quartz. These specimens are often water-worn in riverbeds or coastal areas.
Uses & applications
Used widely in the lapidary arts for cabochons and tumbled stones, decorative landscaping, and as a popular 'healing crystal' in metaphysical circles.
Geological facts
Natural yellow quartz is relatively rare compared to clear quartz. While high-grade Citrine is a precious gemstone, common yellow quartz like this specimen is a staple for rock tumblers because it polishes to a very high shine.
Field identification & locations
Identify in the field by its hardness (cannot be scratched by a steel knife) and its lack of cleavage (it breaks in smooth, curved shell-like patterns). Commonly found in gravel pits, riverbeds, and along beaches in regions with granitic bedrock.
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