
mineral
Native gold specimen (probable gold-bearing quartz)
Native gold, Au, with likely quartz (SiO₂) and possibly iron-oxide/sulfide matrix
AI-generated identification · may be incorrectMetallic yellow-gold luster, irregular to dendritic masses, and no obvious crystal faces; gold is extremely malleable and has Mohs hardness 2.5–3, while quartz is 7. Specific gravity is about 19.3 for pure gold, making it unusually heavy.
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Physical properties
Metallic yellow-gold luster, irregular to dendritic masses, and no obvious crystal faces; gold is extremely malleable and has Mohs hardness 2.5–3, while quartz is 7. Specific gravity is about 19.3 for pure gold, making it unusually heavy.
Formation & geological history
Likely formed by hydrothermal fluids depositing gold in quartz veins or fractures, commonly during orogenic mountain-building events; the specimen’s exact age and locality cannot be determined from the image.
Uses & applications
Used chiefly for jewelry, bullion, electronics, and scientific applications; attractive natural nuggets and matrix specimens are collected. Value depends strongly on verified gold weight, purity, locality, and aesthetics.
Geological facts
Gold’s distinctive color remains yellow in most lighting, unlike pyrite’s brassy, brittle appearance. A streak, density, softness, and professional assay are more reliable than appearance alone.
Field identification & locations
Common sources include Australia, California, Alaska, Nevada, Canada, and South Africa. Test cautiously: gold leaves a yellow streak and deforms under pressure; pyrite powders dark green-black and fractures. Avoid destructive tests without expert supervision.
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