
mineral
Costume Jewelry Gemstones (Emerald-imitation and semi-precious beads)
BeCuAl6Si6O18 (Beryl structure), frequently simulated by glass or synthetic spinel
AI-generated identification · may be incorrectHardness: 7.5-8 (if real Beryl) or 5.5-6 (if glass). Color: Deep green, purple, magenta. Luster: Vitreous. Crystal structure: Hexagonal. Specific gravity: 2.63-2.90.
- Hardness
- 7
- Color
- Deep green, purple, magenta
- Luster
- Vitreous
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Physical properties
Hardness: 7.5-8 (if real Beryl) or 5.5-6 (if glass). Color: Deep green, purple, magenta. Luster: Vitreous. Crystal structure: Hexagonal. Specific gravity: 2.63-2.90.
Formation & geological history
Beryl forms in pegmatites and metamorphic environments where hydrothermal fluids interact with beryllium-rich rocks. Synthetic versions are lab-grown via hydrothermal or flux methods.
Uses & applications
Primarily used in fashion jewelry, beadwork, and personal adornment due to aesthetic appeal.
Geological facts
Emeralds have been prized since antiquity; the oldest were found in Egypt. However, many beads in fashion mixes are treated quartz, dyed agate, or glass.
Field identification & locations
Identify by looking for inclusions under a jeweler's loupe. Natural emeralds have 'jardins' (internal gardens), while imitations may have air bubbles or smooth concave wear patterns typical of glass.
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Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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