
gemstone
Green faceted gemstone, likely emerald or synthetic emerald
Beryl, Be₃Al₂Si₆O₁₈, colored green by chromium and/or vanadium; identity cannot be confirmed visually
AI-generated identification · may be incorrectTransparent to translucent oval faceted stone with vivid bluish-green color and vitreous luster; beryl has Mohs hardness 7.5–8, hexagonal crystal structure, indistinct cleavage, and specific gravity about 2.7.…
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Physical properties
Transparent to translucent oval faceted stone with vivid bluish-green color and vitreous luster; beryl has Mohs hardness 7.5–8, hexagonal crystal structure, indistinct cleavage, and specific gravity about 2.7. Internal fractures/inclusions are visible, but the image cannot distinguish natural from laboratory-grown or simulant material.
Formation & geological history
Natural emeralds form in hydrothermal veins and metamorphic rocks, typically during Precambrian to Mesozoic events; major sources include Colombia, Zambia, Brazil, and Afghanistan. Synthetic emeralds are produced hydrothermally or by flux growth.
Uses & applications
Used primarily in jewelry; lower-quality material is collected as a mineral specimen. Emerald’s value depends strongly on color, clarity, treatment, origin, and laboratory confirmation.
Geological facts
A refractometer, specific-gravity test, loupe examination, and spectroscopy are needed for reliable identification; green glass, synthetic emerald, tourmaline, and other beryl can look similar.
Field identification & locations
Field indicators include strong green color, vitreous luster, and frequent inclusions, but color alone is unreliable. Natural emerald commonly occurs with mica, quartz, feldspar, or calcite in mineralized veins.
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