
Mineral, Metal (element)
Gold
Aurum (Elemental Gold, Au)
Hardness: 2.5-3 on Mohs scale (very soft). Color: Golden yellow, can be reddish or greenish depending on alloys. Luster: Metallic. Crystal Structure: Isometric (typically found as nuggets, flakes, or dendritic masses, not well-formed crystals in nature). Cleavage: None. Ductile and Malleable.…
- Hardness
- 2
- Luster
- Metallic
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Physical properties
Hardness: 2.5-3 on Mohs scale (very soft). Color: Golden yellow, can be reddish or greenish depending on alloys. Luster: Metallic. Crystal Structure: Isometric (typically found as nuggets, flakes, or dendritic masses, not well-formed crystals in nature). Cleavage: None. Ductile and Malleable. Specific Gravity: 19.3 (very high, indicating its density). Chemical Symbol: Au.
Formation & geological history
Gold is typically formed through hydrothermal processes, where hot, mineral-rich fluids circulate through cracks and fissures in the Earth's crust, depositing gold as they cool. It can also be found in placer deposits, where gold eroded from primary deposits is concentrated by water action (e.g., in rivers). Its geological age varies widely as it can form over billions of years, but significant deposits formed during various orogenic (mountain-building) events.
Uses & applications
Industry: Electronics (due to its excellent conductivity and corrosion resistance), dentistry, medical devices. Jewelry: Its unparalleled luster, malleability, and resistance to tarnish make it highly sought after for rings, necklaces, and other ornamental items. Investment: Gold is considered a safe-haven asset and a store of value. Construction: Not typically used.
Geological facts
Gold has been prized by civilizations throughout history for its beauty, rarity, and resistance to corrosion. It is an excellent conductor of electricity and heat. The largest gold nugget ever found, the 'Welcome Stranger' nugget, weighed over 78 kg (2,520 troy ounces) and was found in Australia in 1869. Gold is one of the most unreactive chemical elements.
Field identification & locations
In the field, gold can be identified by its distinctive metallic yellow color, high density (it feels heavy for its size), and malleability (it can be bent or flattened without breaking). It does not tarnish and is non-magnetic. It is commonly found in quartz veins within metamorphic and igneous rocks, and in alluvial (placer) deposits in riverbeds and ancient streambeds. Major gold-producing regions include South Africa, Australia, the United States (Nevada, Alaska), Canada, Russia, and China. For collectors, native gold specimens are highly valued due to their rarity and aesthetic appeal.
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