
mineral
Citrine Quartz Geode
Silicon Dioxide (SiO2) with iron impurities
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Pale yellow to golden honey; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal (pyramidal terminations); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Pale yellow to golden honey
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Pale yellow to golden honey; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal (pyramidal terminations); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed as a secondary mineral in volcanic cavities or hydrothermal veins. While natural citrine is rare, most commercial citrine is created by heat-treating amethyst or smoky quartz to alter iron oxidation states. Typically found in Cenozoic to Precambrian formations.
Uses & applications
Primarily used in jewelry (faceting), crystal healing practices, and as decorative mineral specimens for collectors.
Geological facts
Citrine is known as the 'Success Stone' or 'Merchant's Stone' in folklore. Natural citrine is rare; if a specimen has a white base and a very dark orange tip, it is likely heat-treated amethyst.
Field identification & locations
Identify by hexagonal crystal terminations and lack of cleavage. Found commonly in Brazil, Madagascar, and Russia. When searching in the field, look for quartz points within hollow vugs or geode nodules in igneous landscapes.
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