
mineral
Citrine and Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale; yellow, amber, or brownish-yellow color; vitreous luster; trigonal crystal system; conchoidal fracture with no true cleavage; specific gravity of 2.65.
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Physical properties
Hardness of 7 on the Mohs scale; yellow, amber, or brownish-yellow color; vitreous luster; trigonal crystal system; conchoidal fracture with no true cleavage; specific gravity of 2.65.
Formation & geological history
Formed in igneous, metamorphic, and sedimentary environments, frequently occurring in pegmatites, hydrothermal veins, and as a secondary mineral from the alteration of amethyst via natural heat or irradiation.
Uses & applications
Widely used in jewelry, decorative carvings, metaphysical practices, and as ornamental gemstone pieces for collectors.
Geological facts
Natural citrine is relatively rare compared to heat-treated amethyst, which is commonly sold commercially as citrine. Its yellow color is typically caused by trace amounts of iron impurities and natural irradiation.
Field identification & locations
Identified by its distinctive yellow to brownish-orange color, high hardness, conchoidal fracture, and glassy luster. Commonly sourced from Brazil, Madagascar, Russia, and the United States.
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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