
mineral
Quartz-rich rock, possibly milky quartz
Quartz (silicon dioxide, SiO₂), possibly with feldspar or mica inclusions
AI-generated identification · may be incorrectHardness about 7 Mohs; pale gray to translucent white with vitreous luster, irregular fracture, and no obvious cleavage. The rough, granular appearance suggests quartz-bearing material rather than a cut gemstone.
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Physical properties
Hardness about 7 Mohs; pale gray to translucent white with vitreous luster, irregular fracture, and no obvious cleavage. The rough, granular appearance suggests quartz-bearing material rather than a cut gemstone.
Formation & geological history
Likely formed in a hydrothermal vein or as part of a quartz-rich igneous/metamorphic rock; its exact geological age and setting cannot be determined from the photograph. Quartz veins occur in many regions and geological ages.
Uses & applications
Quartz is used in glass, electronics, abrasives, ceramics, and construction aggregate; attractive pieces are sold as mineral specimens. This specimen appears common and has limited commercial value.
Geological facts
Quartz is one of Earth’s most abundant minerals and forms distinctive six-sided crystals when space permits. The visible yellowish areas may be iron staining or included feldspar rather than gold.
Field identification & locations
Look for glassy luster, hardness sufficient to scratch ordinary glass, and absence of cleavage; a steel nail should not scratch it easily. Common sources include quartz veins, granite, pegmatite, and metamorphic rocks.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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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