mineral

Raw Emerald

Beryl (Be3Al2Si6O18 with Chromium/Vanadium impurities)

Hardness: 7.5-8.0 on Mohs scale; Color: Intense green to bluish-green; Luster: Vitreous to resinous; Crystal system: Hexagonal; Cleavage: Poor/Indistinct; Specific gravity: 2.72-2.78

Hardness: 7
Color: Intense green to bluish-green
Luster: Vitreous to resinous

Identified May 10, 2026More mineral →

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Physical properties

Hardness: 7.5-8.0 on Mohs scale; Color: Intense green to bluish-green; Luster: Vitreous to resinous; Crystal system: Hexagonal; Cleavage: Poor/Indistinct; Specific gravity: 2.72-2.78

Formation & geological history

Forms in pegmatites, hydrothermal veins, and metamorphic rocks. Most high-quality specimens are found in shale-hosted hydrothermal deposits (like Colombia) or mica schists.

Uses & applications

Primarily used as a precious gemstone in jewelry (earrings, rings, necklaces) and as a high-value mineral specimen for collectors.

Geological facts

Emerald is one of the four traditional 'precious' stones. The presence of tiny inclusions, often called 'jardin' (French for garden), is common and often used to verify authenticity and origin.

Field identification & locations

Identify in the field by its characteristic hexagonal crystal habit, hardness, and distinct green color. Common locations include Colombia, Brazil, Zambia, and Ethiopia.

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