
mineral
Gold-bearing quartz sulfide specimen
Native gold (Au) with quartz (SiO₂), likely associated with iron sulfides such as pyrite
AI-generated identification · may be incorrectMetallic yellow grains and gray-white quartz matrix; gold is Mohs 2.5–3, malleable, with a bright metallic luster, while quartz is Mohs 7 and vitreous. The dark metallic material may be pyrite or another sulfide; exact identification requires testing or analysis.
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Physical properties
Metallic yellow grains and gray-white quartz matrix; gold is Mohs 2.5–3, malleable, with a bright metallic luster, while quartz is Mohs 7 and vitreous. The dark metallic material may be pyrite or another sulfide; exact identification requires testing or analysis.
Formation & geological history
Likely formed in hydrothermal veins, where hot mineral-rich fluids deposited quartz, sulfides, and native gold in fractures. The specimen’s geological age cannot be determined from the image and depends on its deposit.
Uses & applications
Gold-bearing specimens are collected for mineral interest and may be assayed for precious-metal content; quartz and sulfides have industrial significance, but this small piece is primarily a specimen rather than construction material.
Geological facts
Native gold is unusually dense and malleable, unlike brassy pyrite, which is brittle and commonly forms cubic crystals. Visual appearance alone cannot establish gold content or value.
Field identification & locations
Commonly found in hydrothermal quartz veins and placer-derived ore zones worldwide. Gold is confirmed by malleability, streak, density, and assay; avoid destructive testing without permission.
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