
mineral
White quartz (likely milky quartz)
Quartz, silicon dioxide (SiO₂)
AI-generated identification · may be incorrectWhite, rough, and somewhat translucent with a glassy-to-dull luster; quartz has Mohs hardness 7, a trigonal crystal structure, and no cleavage, breaking with curved or irregular fracture. The photo does not allow reliable confirmation of the specimen’s identity.
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Physical properties
White, rough, and somewhat translucent with a glassy-to-dull luster; quartz has Mohs hardness 7, a trigonal crystal structure, and no cleavage, breaking with curved or irregular fracture. The photo does not allow reliable confirmation of the specimen’s identity.
Formation & geological history
Quartz commonly crystallizes from silica-rich fluids in veins and cavities or forms in igneous and metamorphic rocks; it occurs in rocks of many geological ages. This small piece’s precise formation history cannot be determined from the image.
Uses & applications
Quartz is used in glassmaking, electronics, abrasives, and decorative objects; milky quartz is also collected and sometimes used in jewelry.
Geological facts
Quartz is one of Earth’s most abundant minerals and is chemically resistant to weathering.
Field identification & locations
Look for hardness sufficient to scratch glass, lack of cleavage, and a white streak; common worldwide in veins, pegmatites, and many rocks. A photo alone cannot distinguish quartz from some other white minerals.
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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