
mineral
Gold Grain
Native Gold (Au)
Hardness: 2.5–3 on Mohs scale; Color: Metallic yellow; Luster: Metallic; Crystal Structure: Isometric (cubic); Cleavage: None; Specific Gravity: 19.3 (very heavy).
- Hardness
- 2
- Color
- Metallic yellow
- Luster
- Metallic
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Physical properties
Hardness: 2.5–3 on Mohs scale; Color: Metallic yellow; Luster: Metallic; Crystal Structure: Isometric (cubic); Cleavage: None; Specific Gravity: 19.3 (very heavy).
Formation & geological history
Formed in hydrothermal quartz veins or as secondary deposits in riverbeds (placer deposits) through erosion of gold-bearing ore. It is chemically inert and does not oxidize.
Uses & applications
Used primarily in jewelry, electronics (conductivity), currency/investment, and medical/dental applications. Small grains are highly sought after by recreational gold prospectors.
Geological facts
Gold is one of the densest minerals on Earth and is incredibly malleable; a single ounce can be beaten into a sheet covering nearly 100 square feet. It is often found associated with quartz and pyrite.
Field identification & locations
Identify in the field by its high density and Sectility (it can be cut or bent without shattering). Unlike pyrite (fool's gold), gold remains bright in shadow and is soft enough to scratch with a copper penny.
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