
mineral
Citrine Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Pale yellow to golden honey-orange, 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 honey-orange, Luster: Vitreous/Glassy, Crystal Structure: Trigonal/Hexagonal, Cleavage: None (Conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Naturally formed through the hydrothermal deposit of silica-rich fluids or the low-grade metamorphism of quartz. Most commercial citrine is created by heating amethyst or smoky quartz to temperatures between 470°C and 560°C.
Uses & applications
Used extensively in the jewelry industry for rings and necklaces, as a healing crystal in metaphysical circles, and for decorative mineral collecting.
Geological facts
Natural citrine is quite rare in nature compared to other quartz varieties. It is known as the 'Success Stone' or 'Merchant's Stone' in folklore. The yellow color is caused by trace amounts of colloidal iron hydroxide.
Field identification & locations
Identify by its characteristic yellow hue and hardness (can scratch glass). Natural citrine is often found in Brazil, Madagascar, and Russia. Unlike heat-treated specimens which often have white bases, natural citrine is uniformly colored through the crystal.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous