
Mineral
Emerald
Beryl (Be₃Al₂Si₆O₁₈), specifically the green variety colored by trace amounts of chromium or vanadium.
Hardness: 7.5-8 on the Mohs scale. Color: Green, ranging from bluish-green to yellowish-green. Luster: Vitreous (glassy). Crystal Structure: Hexagonal. Cleavage: Indistinct. Specific Gravity: 2.67-2.78.…
- Hardness
- 7
- Color
- Green, ranging from bluish-green to yellowish-green
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7.5-8 on the Mohs scale. Color: Green, ranging from bluish-green to yellowish-green. Luster: Vitreous (glassy). Crystal Structure: Hexagonal. Cleavage: Indistinct. Specific Gravity: 2.67-2.78. Often contains inclusions, known as 'jardin' (French for garden), which are typically considered acceptable and sometimes even desirable as they attest to a natural origin.
Formation & geological history
Emeralds are typically formed in low-temperature hydrothermal veins and pegmatites, often associated with metamorphic rocks like schists and contact metamorphic deposits. The characteristic green color comes from trace elements like chromium or vanadium replacing aluminum in the beryl crystal lattice. The specific geological age varies widely depending on the deposit, with some being hundreds of millions of years old (e.g., Colombian emeralds) and others younger.
Uses & applications
Emerald is one of the four precious gemstones (along with diamond, ruby, and sapphire) and is highly valued in jewelry. Although less commonly used, lower quality or industrial-grade beryl (not necessarily emerald) can be a source of beryllium metal, used in alloys, aerospace, and nuclear industries.
Geological facts
Emeralds have been prized since ancient times. Legend has it they were Cleopatra's favorite gemstone. The largest emerald ever found is the 'Teodora' (meaning 'Gift of God'), weighing 11.5 kg (57,500 carats). Emeralds are often treated with oils or resins to improve their clarity and fill surface-reaching fractures, a common and accepted practice in the gemstone industry.
Field identification & locations
In the field, raw emerald crystals typically form as hexagonal prisms. The vibrant green color is the most obvious identifier, distinguishing it from other green minerals like peridot, tsavorite garnet, or diopside. However, due to its value, proper identification often requires gemological testing to differentiate from simulants or other beryls. Major sources include Colombia (known for its fine-quality emeralds), Brazil, Zambia, Afghanistan, and Russia. When purchasing, look for a strong, vivid green color, transparency, and minimal visible inclusions (though some are expected). Collectors often seek well-formed crystals with good color.
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