
mineral
Yellow Quartz / Citrine Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Honey-yellow to light yellowish-brown; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None, exhibits conchoidal fracture; Specific Gravity: ~2.65.
- Hardness
- 7 on Mohs scale
- Color
- Honey-yellow to light yellowish-brown
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Honey-yellow to light yellowish-brown; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None, exhibits conchoidal fracture; Specific Gravity: ~2.65.
Formation & geological history
Formed in igneous pegmatites, hydrothermal veins, and metamorphic rocks. Yellow color is typically caused by ferric iron impurities or natural irradiation within the silicon dioxide crystal lattice.
Uses & applications
Widely used as an gemstone in jewelry, decorative stone carvings, lapidary projects, and popular among mineral collectors.
Geological facts
Natural citrine is relatively rare in nature. Many commercial citrines are produced by heat-treating amethyst or smoky quartz, but natural yellow quartz formed in pegmatite veins retains a soft, honey-like translucency.
Field identification & locations
Identify by its hardness (scratches glass easily, cannot be scratched by a steel blade), greasy to vitreous luster, lack of cleavage, and translucent yellow-brown coloration. Commonly found in Brazil, Madagascar, and Russia.
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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
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary