
mineral
Orange Quartz (Citrine Quartz)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Rusty orange/amber to yellow; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Rusty orange/amber to yellow
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Rusty orange/amber to yellow; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in igneous or metamorphic environments when silica-rich hydrothermal fluids cool and crystallize. The orange hue is caused by colloidal iron hydroxide (limonite) staining or internal iron impurities.
Uses & applications
Used in the gemstone and jewelry trade, lapidary arts (cabochons), and highly prized by metaphysical collectors. Industrial grade quartz is used in glassmaking and electronics.
Geological facts
Natural citrine is rare; many specimens are actually heat-treated amethyst. This specific jagged, iron-stained specimen is common in gravel deposits and riverbeds. Quartz is the second most abundant mineral in Earth's continental crust.
Field identification & locations
Identify by its ability to scratch glass and lack of cleavage planes. Found globally in pegmatites and metamorphic veins. Collectors look for translucency and vibrancy of color.
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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