
mineral
Emerald (Faceted Gemstone)
Beryl (Be3Al2Si6O18 with Chromium/Vanadium impurities)
AI-generated identification · may be incorrectHardness: 7.5-8.0 (Mohs); Color: Vivid green to bluish green; Luster: Vitreous; Crystal Structure: Hexagonal; Cleavage: Imperfect; Specific Gravity: 2.67-2.78.
- Hardness
- 7
- Color
- Vivid green to bluish green
- Luster
- Vitreous
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Physical properties
Hardness: 7.5-8.0 (Mohs); Color: Vivid green to bluish green; Luster: Vitreous; Crystal Structure: Hexagonal; Cleavage: Imperfect; Specific Gravity: 2.67-2.78.
Formation & geological history
Formed in hydrothermal veins or pegmatites where beryllium-rich fluids interact with chromium or vanadium-rich rocks. Geological age varies from 30 million to 2.9 billion years old depending on the locality.
Uses & applications
Primarily used as a precious gemstone in high-end jewelry and for investment-grade mineral collections.
Geological facts
Emeralds are the birthstone for May. Unlike rubies or sapphires, almost all natural emeralds contain inclusions (referred to as a 'jardin'), making flawless stones extremely rare.
Field identification & locations
Identified in the field by its distinct green color and hexagonal prism crystal habit. Key locations include Colombia, Brazil, Zambia, and Ethiopia. Testing for refractive index and specific gravity is required to distinguish from lookalikes like tsavorite garnet or green glass.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary