
mineral
Iron-stained quartz-rich rock, possibly smoky quartz
Quartz (SiO₂), likely with iron-oxide staining and dark inclusions; exact identification is uncertain from the photo
AI-generated identification · may be incorrectHardness 7 Mohs; brown to gray, translucent in places, with a vitreous luster and irregular fracture. The apparent granular texture may indicate quartz in a matrix rather than a single crystal; no clear cleavage is visible.
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Physical properties
Hardness 7 Mohs; brown to gray, translucent in places, with a vitreous luster and irregular fracture. The apparent granular texture may indicate quartz in a matrix rather than a single crystal; no clear cleavage is visible.
Formation & geological history
Likely formed in a hydrothermal vein or pegmatitic environment, where silica-rich fluids deposited quartz and later oxidation produced reddish-brown iron staining. A precise geological age cannot be determined visually.
Uses & applications
Common quartz is used in glass, ceramics, abrasives, electronics, and countertops; attractive pieces may be sold as mineral specimens. This specimen appears more suitable for casual collecting than jewelry.
Geological facts
Quartz is one of Earth’s most abundant minerals and is piezoelectric, producing an electrical charge under pressure. The dark material could be inclusions or attached host rock, not necessarily smoky quartz.
Field identification & locations
Look for glassy luster, conchoidal fracture, lack of cleavage, and resistance to scratching with a steel blade; quartz should scratch glass. Common worldwide, especially in hydrothermal veins and pegmatites.
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