
mineral
Quartz (Citrine or Iron-stained variety)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: yellowish-brown to amber; Luster: vitreous (glassy) to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: none (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- yellowish-brown to amber
- Luster
- vitreous (glassy) to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: yellowish-brown to amber; Luster: vitreous (glassy) to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: none (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or as a secondary mineral in volcanic cavities (geodes). The yellow tint is often caused by submicroscopic iron impurities or natural radiation within the earth.
Uses & applications
Used in jewelry (gemstone), electronics for its piezoelectric properties, glass manufacturing, and as a popular decorative specimen for collectors.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Most commercial citrine is actually heat-treated amethyst or smoky quartz, but natural yellow quartz found in the wild is often colored by iron oxides.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and glassy appearance on broken surfaces. Commonly found in riverbeds, mountain regions, and tailings from old mines.
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