
mineral
Native Gold Nuggets
Native Gold (Au)
AI-generated identification · may be incorrectHardness: 2.5-3 (Mohs scale); Color: Metallic gold-yellow; Luster: Metallic; Crystal structure: Isometric (though usually occurs as irregular nuggets or grains); Cleavage: None; Specific Gravity: 15.5-19.3 (very high density).
- Hardness
- 2
- Color
- Metallic gold-yellow
- Luster
- Metallic
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Physical properties
Hardness: 2.5-3 (Mohs scale); Color: Metallic gold-yellow; Luster: Metallic; Crystal structure: Isometric (though usually occurs as irregular nuggets or grains); Cleavage: None; Specific Gravity: 15.5-19.3 (very high density).
Formation & geological history
Formed primarily in hydrothermal quartz veins via precipitation from hot, mineral-rich fluids. Nuggets like these are often found in placer deposits, where erosion has moved the gold from its primary source into riverbeds (alluvial) and concentrated it due to its high density.
Uses & applications
Dominantly used as a store of value (investment), in jewelry making, and in high-end electronics due to its excellent conductivity and corrosion resistance. Small nuggets are highly prized by mineral collectors.
Geological facts
Gold is incredibly ductile; a single ounce can be beaten into a sheet covering 100 square feet. It is one of the few elements found in its 'native' or pure metallic state in nature. These specific specimens show the rounded, water-worn texture typical of stream-found gold.
Field identification & locations
Identify in the field by its high density (it feels much heavier than it looks), malleability (it will dent or bend under pressure rather than shatter like pyrite), and its persistent yellow color regardless of the lighting angle. Commonly found in areas with historic volcanic or tectonic activity like California, Alaska, and Australia.
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