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Emerald

Beryl

By Tim Matthews, JD, FGA, GG, DGA,
CEO and President of JTV (retired)
Published: June 2014
Modified: February 2024
Emerald Polished Emerald Rough Emerald Jewelry
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Need emerald in your gem collection? Shop gemstones.com on Jedora.
Table of Contents
  • General Information
  • Emerald Colors
  • Emerald Spectra
  • Countries of Origin
  • History
  • Care
  • More About Emerald
  • Pattern
  • Creation Method
  • Enhancement
  • Related Videos

Emerald is a beryllium aluminum silicate that owes its color to trace amounts of chromium or vanadium (or both) and, sometimes iron. Stones must have sufficient tone and saturation to be considered emerald. Emerald is the birthstone for May and is considered one of “The Big Three” along with ruby and sapphire. Although attempts at emerald synthesis began in the 1880’s, it was not until the 1930s that a synthetic emerald would be produced in a quality and quantity high enough to be commercially marketable.

General Information

  • Classification
  • Optical Properties
  • Characteristic Physical Properties
  • Chemistry & Crystallography
Common Name
Emerald
Species
Beryl
Transparency
Transparent - Translucent
Dispersion
Strength: Weak Fire Value: 0.014
Refractive Index
1.577-1.600
Tolerance:(+0.017/-0.017)
Birefringence
0.005-0.009
Optic Character
Uniaxial
Optic Sign
Negative
Polariscope Reaction
Doubly Refractive (DR)
Fluorescence
SWUV: Inert to weak orangy red to red
LWUV: Inert to strong orangy red to red
CCF Reaction
Some appear pink or red; not diagnostic.
Pleochroism
Dichroic, moderate to strong, varying shades of body color
Hardness
7.5
Streak
White
Specific Gravity
2.670-2.900 Range:0.18/-0.05 Typical:2.72
Toughness
Poor
Inclusions
Emerald is a type III clarity stone. 3-phase inclusions typical of Colombian material. 2-phase inclusions usually found in stones from India. Tremolite needles are typical of Zimbabwe stones. Actinolite needles can be found in Siberian stones. Emeralds sometime have tube-like and bamboo-like inclusions, liquid and fingerprint inclusions, calcite, pyrite, mica, needles and amphibole inclusions.
Luster
Vitreous
Stability
Fair
Fracture
Conchoidal
Cleavage
Poor, in one direction
Chemical Name
beryllium aluminum silicate
Chemical Formula
Be3Al2(SiO3)6
Crystal System
Hexagonal
Chemistry Classification
Silicate

Emerald Colors

  • Green Emerald
    Green
  • Green Emerald
    Green
  • Green Emerald
    Green
  • Green Emerald
    Green

Emerald Spectra

Emerald Spectra
EMERALD GILSON FLUX SYNTHETIC E RAY

As the e ray is isolated the more bluish green color is seen in the body color of the stone and the spectrum reacts accordingly. The main absorption band has moved further to the long wave side to obscure the line at 637nm. The line at 662nm. and the doublet at 680/683nm. are present but not as strong as in deeper colored emeralds. The line in the blue at 477nm. is not present on this ray.

Emerald Spectra
EMERALD LENNIX Lab Created (Unpolarized)

Color mainly due to chromium. The absorption spectra is essentially the same for that of natural Emerald.

Emerald Spectra
EMERALD LENNIX Lab Created  (ω ray)

The o ray spectrum is typical of most emeralds of this color saturation with the feature of the line in the blue at 477nm. although in this case a little difficult to detect as absorption sets in around this point. The line in the orange- red at 637nm. has strengthened and the doublet is weaker as the o ray assumes its more yellowish green color.

Emerald Spectra
EMERALD LENNIX Lab Created (ε-ray)

Color mainly due to chromium. The absorption spectra is essentially the same for that of natural Emerald. The line at 637nm has now disappeared, covered by the main absorption band which has moved further to the long wave side allowing the line at 662nm. to be seen. The line sometimes seen at 646 nm. remains hidden by the main band. The shift in absorption and the absence of the line in the blue accounts for the more bluish green of the e ray.

Emerald Spectra
EMERALD GILSON FLUX SYNTHETIC unpolarized

Color mainly due to chromium. As the color saturation becomes less, so does the strength of absorption. The main feature is the central absorption band is weaker and narrower and the other lines are noticeably weaker.

Emerald Spectra
EMERALD GILSON FLUX SYNTHETIC O RAY

The dichroism in this stone is more pronounced as the o ray assumes it's more yellowish green color. The o ray spectrum is typical of most emeralds of this color saturation with the feature of the line in the blue at 477nm. but rather weak and not easily detected. The central area of absorption has strengthened and widened. Other lines are weaker.

We acknowledge the significant scientific contributions of John S Harris, FGA to the study of gemstone spectra and with deep appreciation to him, acknowledges the use of his images and related notes about gemstones and their spectra in the educational materials on this website.

Countries of Origin

Tanzania, United Republic Of; Afghanistan; Russian Federation; Cambodia; Czechia; United States of America; Egypt; Somalia; Madagascar; Kazakhstan; Thailand; Portugal; Austria; Mozambique; Pakistan; Unknown; China; Brazil; Bulgaria; Chile; France; Nigeria; Colombia; Argentina; Romania; Sri Lanka; Rwanda; Ukraine; Zambia; Switzerland; Bolivia (Plurinational State of); India; Spain; Canada; Norway; Namibia; Italy; Mexico; South Africa; Zimbabwe; Australia; Peru; Ethiopia; Germany; Greenland

History

Emerald is the stone that sets the standard by which all green gemstones are measured. The most-famous member of the beryl family, emerald is prized for its variety of greens, often with secondary blue or yellow hues. From deep, rich greens to the palest, springtime pastels, emerald has the perfect color for the green-lover in you. Emeralds get their green from chromium, vanadium, or both. There are other elements that color beryl green, but only those colored by chromium and vanadium are classified as emeralds. In his epic work, Natural History, the Roman historian Pliny the Elder stated of emeralds, "The sight of no other color is more agreeable... because nothing greens greener."

Care

Emeralds are also known for their jardins, French for "gardens" - inclusions intrinsic to each stone and which make every stone unique. Almost all emeralds are oiled. Treat your emerald like the special stone it is - no harsh chemicals, steam, or sonic cleaning. Warm sudsy water will keep it looking its best.

Emerald Gemstone

More About Emerald

To the ancient Romans, emerald symbolized the reproductive forces of nature. To the early Christians, emerald represented resurrection. No stone with the glory of color that is emerald could be thought to be less than magical! According to Marbode, writing in the 11th century, "emerald improves memory, makes its owner eloquent and persuasive, and brings him joy." We can't confirm eloquence or persuasion... but we can certainly affirm joy!

Pattern

Trapiche

Trapiche emeralds hail exclusively from the emerald mines in the Boyac region of Colombia, and are so named because their patterns resemble the spoked wheels of the heavy gear locals use to grind sugar cane. Extremely limited in supply, trapiche emeralds are perhaps the rarest of all "pattern" gemstones. Their six distinct "spokes" are caused by the presence of the mineral inclusion lutite. As the hexagonal emerald crystal grew, it pushed the lutite towards the center of the crystal and then radiated out in the six directions of the emerald crystal. A truly remarkable feat, compliments of Mother Nature!

Trapiche Emerald
Trapiche Emerald
  • Classification
  • Optical Properties
Common Name
Trapiche
Refractive Index
1.560-1.570
Fluorescence
SWUV: Inert
LWUV: Inert
Pleochroism
Dichroic, weak to moderate, varying shades of body color

Creation Method

Lab Created Overgrowth Hydrothermal

One of the most popular methods for creating emerald is the hydrothermal process, which uses heat and pressure to imitate natural conditions deep in the earth that formed natural gems. Nutrients are dissolved in a water solution with synthetic crystals forming as the solution cools. Synthetic emeralds offer you the best of both worlds. You get the beauty of a beloved, rare gemstone, but at a budget-friendly price!

  • Classification
  • Optical Properties
  • Characteristic Physical properties
Common Name
Lab Created Overgrowth Hydrothermal
Refractive Index
1.566-1.570
Fluorescence
SWUV: Weak to moderate red in the synthetic layer
LWUV: Moderate to strong red in the synthetic layer
CCF Reaction
Often a bright red; not conclusive
Toughness
Good

Hydrothermal

Hydrothermally grown synthetic emeralds crystallize slowly out of a solution (a mix of water and dissolved elements) that has been exposed to heat and pressure similar to the conditions on Earth under which the natural gem mineral grows. Synthetic gems have the same chemical, optical, and physical properties of their natural counterparts, but are a more cost-effective alternative to a natural gem.

Hydrothermal Emerald
Hydrothermal Emerald
  • Classification
  • Optical Properties
  • Characteristic Physical properties
Common Name
Hydrothermal
Refractive Index
1.571-1.584
Tolerance:(+0.007/-0.002)
Birefringence
0.004-0.008
Fluorescence
SWUV: Variable
LWUV: Variable
CCF Reaction
Sometimes bright red; not conclusive
Specific Gravity
2.63
Stability
Good

Sandwich Hydrothermal

Synthetic refers to a man-made material with a natural counterpart. The synthetic crystal replicates the chemical, optical and physical properties of the natural crystal with little or no variation. One of the most popular methods for creating synthetic emerald is the hydrothermal process, which uses heat and pressure to imitate natural conditions deep in the earth that formed natural gems. Nutrients are dissolved in a water solution with synthetic crystals forming as the solution cools. Synthetic emeralds offer you the best of both worlds. You get the beauty of a beloved, rare gemstone, but at a budget-friendly price!

  • Classification
  • Optical Properties
  • Characteristic Physical properties
Common Name
Sandwich Hydrothermal
Refractive Index
1.575-1.581
Birefringence
0.004-0.004
Fluorescence
SWUV: Moderate to strong red
LWUV: Moderate to strong red
CCF Reaction
Often a bright red; not conclusive
Stability
Good

Flux Growth

One method of synthesizing emeralds is called flux growth. During the flux growth process, flux, a substance that reduces the melting point of surrounding material, is combined in a metal-lined crucible with the elements that make up emerald. The crucible is heated until its contents are liquid and then it is allowed to cool very slowly. As cooling continues, the gem mineral crystallizes from the solution. Flux grown synthetic gems can take up to a year to grow to a facetable size, but the exceptional clarity of these gems is well worth the wait! Synthetic gems have the same chemical, optical, and physical properties of their natural counterparts, but are a more cost-effective alternative to a natural gem.

Flux Growth Emerald
Flux Growth Emerald
  • Classification
  • Optical Properties
  • Characteristic Physical properties
Common Name
Flux Growth
Refractive Index
1.562-1.569
Tolerance:(+/-0.003)
Birefringence
0.003-0.005
Fluorescence
SWUV: Variable
LWUV: Variable
CCF Reaction
red
Specific Gravity
2.66
Stability
Good

Enhancement

Fractured-Filled

Fracture filling is the filling of surface-breaking cavities or fissures with highly refractive colorless glass. This process may improve the appearance, durability and/or weight of the emerald.

Fractured-Filled Emerald
Fractured-Filled Emerald
  • Classification
  • Optical Properties
Common Name
Fractured-Filled
Fluorescence
SWUV: Variable
LWUV: Variable

Related Videos

All About May's Emerald (source: JTV YouTube)
Shop for gorgeous green emeralds through gemstones.com on Jedora.
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