Native Gold
Chemical formula: Au
Native gold is a naturally occurring elemental noble metal, valued for its color, corrosion resistance, and malleability.
Properties
- Mohs hardness
- 2.5-3
- Luster
- Metallic
- Streak
- Shining yellow
- Density
- 15
- Cleavage
- None
- Fracture
- Haczykowaty
- Transparency
- Opaque
- Crystal system
- Isometric
Diagnostic features
## Identification Native gold can be identified by its characteristic, intensely yellow color, strong metallic luster, and high density. It is very soft and malleable, and can be scratched with a copper wire or knife. Its streak is shiny yellow. It often occurs as irregular flakes, wires, or nuggets. ## Distinguishing from Similar Minerals Gold is sometimes confused with pyrite ("fool's gold") or chalcopyrite. Pyrite has a brighter, brassy-yellow color, is much harder (6-6.5 on the Mohs scale), brittle, and has a black streak. Chalcopyrite has a more greenish-yellow hue, is also harder and brittle. Gold differs from them in its malleability, softness, and shiny yellow streak. ## Crystal Forms Gold crystals are rare, but if they occur, they usually have an octahedral, rhombic dodecahedral, or cubic habit. More often, it is found as irregular nuggets, flakes, wires, fibers, dendrites, or granular aggregates, forming nuggets.
Geological environment
## Genesis Native gold forms in hydrothermal processes associated with volcanic activity and magmatic intrusions. Hot gold-rich solutions circulate in rock fractures, where, due to changes in pressure and temperature, gold precipitates and crystallizes. It also occurs in secondary, so-called placer (alluvial) deposits, where it is concentrated in river and glacial sediments as a result of the erosion of primary deposits. ## Mineral Associations Native gold often co-occurs with quartz, pyrite, chalcopyrite, arsenopyrite, galena, sphalerite, as well as other ore minerals and sulfides. In placer deposits, it is accompanied by heavy minerals such as magnetite, ilmenite, and garnets. ## Localities Significant deposits of native gold occur worldwide. Important historical and contemporary localities include: Witwatersrand in South Africa, Kalgoorlie in Australia, the Klondike region in Canada, Sierra Nevada in California (USA), the Urals in Russia, and numerous places in Brazil and China.
Rarity
Very Common
For collectors
## Quality Criteria The most prized specimens of native gold are well-formed crystals, especially those with distinct faces and forms. Large nuggets of interesting shapes, free from impurities and damage, are also highly sought after. Specimens with visible inclusions of quartz or other minerals can be attractive due to their aesthetics and geological context. An intense, pure yellow color is also an important criterion. ## Popular Localities The most prized gold specimens come from historical and contemporary mining regions such as California (USA), Australia (e.g., Victoria, Kalgoorlie), Colombia, Brazil, Russia (Urals), and Canada (Klondike).
Care and storage
## Cleaning Native gold can be cleaned gently using a soft brush and warm water with a small amount of mild soap. After washing, rinse the specimen thoroughly with clean water and dry with a soft cloth to avoid deposits. ## What to Avoid Avoid using aggressive chemicals, such as strong acids or bases, which can damage the surface of the gold or contaminate other minerals with which gold may co-exist. Gold is soft, so it should be protected from scratches and impacts. It is not sensitive to sunlight or typical temperature changes, but extreme conditions can affect accompanying minerals. ## Storage Gold specimens are best stored in individual, soft pouches or in padded boxes to prevent scratches. Due to its value, it is recommended to store it in a safe place, away from moisture, which could promote corrosion of other metals in the case of alloys.