
mineral
Yellow Quartz (Citrine-colored Quartz)
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale), Color: Pale yellow to golden, Luster: Vitreous/Glassy, Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Pale yellow to golden, Luster: Vitreous/Glassy, Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Formed in igneous pegmatites or hydrothermal veins where silicon-rich fluids crystallize. Its yellow tint often comes from trace amounts of ferric iron or natural irradiation during high-temperature formation.
Uses & applications
Commonly used in jewelry (as tumbled stones or faceted gems), ornamental carvings, crystal healing collections, and as a source of silicon for electronic components.
Geological facts
Much of the darker yellow quartz on the market is actually heat-treated amethyst. Natural pale yellow quartz, like this specimen, is more common in its raw tumbled form.
Field identification & locations
Identify by its hardness (it will scratch glass) and lack of cleavage. Look for internal veining or 'clouds' common in macroscopic quartz. Found worldwide, with major deposits in Brazil and Madagascar.
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