
mineral
Quartz-rich rock, possibly milky quartz in a weathered host
Quartz (SiO₂); the specimen may be a quartz vein fragment, but the image is insufficient for a precise identification
AI-generated identification · may be incorrectPale cream to white, opaque to slightly translucent, with a vitreous-to-dull surface; quartz hardness is 7 Mohs and its crystals are hexagonal with no cleavage. The rough, weathered specimen obscures its full texture and composition.
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Physical properties
Pale cream to white, opaque to slightly translucent, with a vitreous-to-dull surface; quartz hardness is 7 Mohs and its crystals are hexagonal with no cleavage. The rough, weathered specimen obscures its full texture and composition.
Formation & geological history
Quartz commonly forms when silica-rich fluids fill cracks and crystallize as veins in many rock types; vein formation can occur across a wide range of geological ages.
Uses & applications
Quartz is used in glass, electronics, abrasives, and construction aggregate; attractive pieces may be collected or cut, though this specimen appears unworked.
Geological facts
Quartz is one of Earth’s most abundant minerals and breaks with a curved, conchoidal fracture rather than cleavage.
Field identification & locations
Look for hardness sufficient to scratch glass, a glassy appearance on fresh surfaces, and no cleavage; quartz veins are common worldwide. The visible specimen could include other minerals, so a close examination is needed to identify the host rock.
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