
mineral
Tumbled yellow-brown quartz (likely citrine or iron-stained quartz)
Quartz, SiO₂; yellow color may result from iron impurities
AI-generated identification · may be incorrectTranslucent honey-yellow to brown, glassy luster, irregular internal clouding; Mohs hardness 7, trigonal crystal structure, no true cleavage. The image does not show diagnostic crystal faces, so the exact variety cannot be confirmed visually.
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Physical properties
Translucent honey-yellow to brown, glassy luster, irregular internal clouding; Mohs hardness 7, trigonal crystal structure, no true cleavage. The image does not show diagnostic crystal faces, so the exact variety cannot be confirmed visually.
Formation & geological history
Quartz crystallizes from silica-rich fluids in veins and cavities; iron staining or heat treatment can produce yellow-brown color. Quartz occurs in rocks of many ages.
Uses & applications
Used for jewelry, ornaments, and collecting; quartz is also important in glassmaking and electronics.
Geological facts
Natural citrine is relatively uncommon; much commercial material sold as citrine is heat-treated amethyst or iron-bearing quartz.
Field identification & locations
A scratch test and examination under magnification can help distinguish quartz from softer look-alikes; common worldwide in veins and pegmatites. Its smooth shape suggests it has been tumbled or naturally water-worn.
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Sandstone (with potential mineral staining/concretions)
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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)
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