
mineral
Citrine (Quartz variant)
SiO2 (Silicon Dioxide)
AI-generated identification · may be incorrectHardness: 7.0 on Mohs scale; Color: Pale yellow to golden-orange; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7
- Color
- Pale yellow to golden-orange
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7.0 on Mohs scale; Color: Pale yellow to golden-orange; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in igneous (pegmatites) or metamorphic environments through crystallization. Most commercial citrine is produced by heat-treating Amethyst or Smoky Quartz at approximately 470°C to 560°C. Natural citrine is rare.
Uses & applications
Primary use is in jewelry as a gemstone (birthstone for November); decorative carvings; and as a common specimen for crystal collection and metaphysical purposes.
Geological facts
Naturally occurring citrine is extremely rare. Almost all 'citrine' in the global market is heat-treated amethyst, identifiable by its reddish tint and white bases. Natural citrine is usually a pale 'lemon' yellow.
Field identification & locations
Identify by its hardness (scratches glass), lack of cleavage, and transparent golden honey color. Commonly found in Brazil, Madagascar, and Russia. Collectors look for clarity and absence of brownish zones.
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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