
mineral
Gold-bearing quartz vein rock
Quartz (SiO₂) with probable native gold and iron-oxide minerals
AI-generated identification · may be incorrectHardness about 7 for quartz; gray-white, yellow-brown, granular and locally glassy, with dull to vitreous luster. The yellow metallic-looking flecks may be native gold, but could also be pyrite or iron staining; crystal structure is trigonal quartz with no cleavage.
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Physical properties
Hardness about 7 for quartz; gray-white, yellow-brown, granular and locally glassy, with dull to vitreous luster. The yellow metallic-looking flecks may be native gold, but could also be pyrite or iron staining; crystal structure is trigonal quartz with no cleavage.
Formation & geological history
Likely hydrothermal quartz deposited in fractures, with later oxidation producing brown iron oxides; associated gold formed during the same mineralizing event. Its exact geological age and locality cannot be determined from the image.
Uses & applications
Gold-bearing quartz is primarily an ore and collecting specimen; quartz itself is used in glass, ceramics, abrasives, and electronics. Attractive pieces may be displayed, but this specimen is not gem quality.
Geological facts
Visible yellow material cannot be reliably identified as gold photographically; gold is very soft, malleable, and does not form sharp brittle cubic crystals, unlike pyrite. A streak, hardness, density, and professional assay are needed for confirmation.
Field identification & locations
Common in hydrothermal veins, especially around ancient volcanic and metamorphic terranes. Test suspected gold with a steel pin or knife (gold deforms rather than crumbles), inspect with a loupe, and obtain an assay before assigning value.
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