
mineral
Citrine Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Yellow to brownish-orange, Luster: Vitreous (glassy), Crystal Structure: Hexagonal (trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Yellow to brownish-orange, Luster: Vitreous (glassy), Crystal Structure: Hexagonal (trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Formed in igneous and metamorphic environments, specifically in pegmatites or hydrothermal veins. Natural citrine is rare and often forms when amethyst or smoky quartz is subjected to natural heat from the Earth's crust.
Uses & applications
Predominantly used as a gemstone in jewelry, as well as for lapidary decor, crystal healing collections, and industrial glass production in its impure forms.
Geological facts
Natural citrine is quite rare; most 'citrine' on the market is actually heat-treated amethyst or smoky quartz. One of the largest faceted citrines weighs over 20,000 carats and is known as the Malaga Citrine.
Field identification & locations
Identify by its hardness (scratches glass) and lack of cleavage. In the field, look for hexagonal prismatic crystals. Major deposits are 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
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