
mineral
Rough Citrine Quartz
Silicon Dioxide (SiO2) with ferric iron impurities
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Pale yellow to smoky amber; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Pale yellow to smoky amber
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Pale yellow to smoky amber; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed in igneous or metamorphic environments, primarily within hydrothermal veins or pegmatites. Natural citrine is rare and often forms when amethyst or smoky quartz is subjected to natural geothermal heat.
Uses & applications
Primarily used in jewelry as a gemstone and by mineral collectors. In industry, quartz is used for its piezoelectric properties in electronics, though synthetic versions are more common for that purpose.
Geological facts
Known as the 'Success Stone' or 'Merchant's Stone' in folklore. Most commercial citrine is actually heat-treated amethyst, which takes on a deep orange hue, whereas natural citrine is typically a paler yellow.
Field identification & locations
Identify in the field by its hardness (scratches glass), glassy luster, and absence of cleavage planes. Common locations include Brazil (the top producer), Madagascar, Spain, and Russia. Look for it in river beds near quartz veins.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
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Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
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