
mineral
Gold-bearing Quartz Ore
Auriferous Quartz (SiO2 with Au)
AI-generated identification · may be incorrectHardness: 7 (Quartz) / 2.5-3 (Gold); Color: Milky to vitreous gray quartz with metallic yellow inclusions; Luster: Vitreous to metallic; Crystal structure: Trigonal/Isometric; Specific Gravity: 2.65 (Quartz) / 19.3 (Gold)
- Hardness
- 7 (Quartz) / 2
- Luster
- Vitreous to metallic
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Physical properties
Hardness: 7 (Quartz) / 2.5-3 (Gold); Color: Milky to vitreous gray quartz with metallic yellow inclusions; Luster: Vitreous to metallic; Crystal structure: Trigonal/Isometric; Specific Gravity: 2.65 (Quartz) / 19.3 (Gold)
Formation & geological history
Formed in hydrothermal veins when hot, mineral-rich fluids circulate through fractures in the Earth's crust, often during orogenic (mountain-building) events. Most significant deposits range from Precambrian to Cenozoic.
Uses & applications
Primary source for industrial gold production, jewelry, electronics, and highly prized by mineral collectors as 'specimen gold'.
Geological facts
Quartz is the most common host mineral for gold. Historically, 'Quartz Mining' refers to lode mining where the host rock must be crushed to extract the precious metal, unlike placer mining in rivers.
Field identification & locations
Identify by looking for high-density metallic yellow flecks that do not shatter when poked with a needle (unlike pyrite) within translucent or white quartz veins. Common in California, Alaska, Australia, and South Africa.
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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
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Granite
Granite (Phaneritic intrusive igneous rock)
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