
mineral
Yellow Quartz (Citrine Quartz or Yellow Chalcedony)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Pale yellow to honey-brown, Luster: Vitreous (glassy) to waxy when tumbled, Crystal Structure: Trigonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Pale yellow to honey-brown, Luster: Vitreous (glassy) to waxy when tumbled, Crystal Structure: Trigonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Formed through the cooling and crystallization of silica-rich hydrothermal fluids in veins or cavities within igneous and metamorphic rocks. Many yellow quartz specimens are naturally heated by geothermal activity.
Uses & applications
Used primarily in jewelry casting, crystal collections, lapidary work, and sometimes as an abrasive in industrial applications.
Geological facts
Natural citrine is rare; much of the bright yellow-orange quartz sold commercially is actually heat-treated amethyst. This specimen appears to be a natural river-worn or tumbled yellow quartz pebble.
Field identification & locations
Identify by its ability to scratch glass (hardness 7) and its lack of cleavage. Commonly found in riverbeds or near granitic intrusions. Collectors look for clarity and consistent color saturation.
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Gneiss or Schist
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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