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COUNTRY NAME ADDRESS CITY ZIP CODE
         
Australia Gemmological Association of Australia Queensland Branch, 20 Rosslyn Street, East Brisbane Quensland 4169
  Gemmological Association of Australia South Australia Branch, G.P.O Box 5133 AA Melbourne  
Belgium European Gemological Laboratory Rijfstraat 3 Antwerp  
  HRD Institute of Gemology Diamond High Council Antewerp  
Brazil Universidad Federal de Oro Preto Escola de Minas, Praca Tiradentes, 20 Oro Preto MG 35400
Canada Carleton University Otawa Ontario K1S5B6
  George Brown College of Applied Arts & Techonology P.O Box 1015 Station B, Toronto Ontario M5T2T9
  Pacific Institute of Gemology P.O Box 6902, Vancouver, BC Vancouver V5k4W3
  Canadian Gemmolgical Association 1767 Avenue Road, North York Ontario M5M3Y8,
England Departament of Mineralogy British Museum (Natural History) Cromwell Rd. London SW75BD,
  Gemologiacal Association of Great Britain 2 Carey Lane London EC2,
  Gemmological Laboratory Benedict Building St, George´s Way, Stocton Road Sunderland SR27BW,
  Huddlestone Gemmological Consultants Ltd 100 Hatton Garden Suite 221 London ECIN8NX,
France Institut de Gemmologie (ING) 48 Rue Due Faubourg Montmartre Paris 75009
Germany Deutsche Gemmologische Gesellschaft Prof. Schlossmacher-Str.1, P.O Box 12 22 60 Idar-Oberstain D6580
Hong Kong G.I.A Hong Kong Unit # 1211B, 12/f, Block A, Focal Industrial Center, 21 Man Lock Street, Hunghom Kowloon Hong Kong  
  The Hong Kong Institute of Gemmology 1104 Blissful Building, 247 Des Voeux Road Central Hong Kong  
  The Gemmological Association of Hong Kong TST P.O Box 89771, Kowloon Hong Kong  
Israel E.G.L Gemological Institute for Precious Stones Noam Bldg, Bezalel St.52 Ramat Gan  
  Gemmological Association of Israel 1 Jabotinsky St. Ramat Gan 52520,
Italy G.I.A S.R.L (Italy) Via Vecchia Ferriera 70 Vicenza 36100
  Instituto Gemmologico Mediterraneo Via Marmolaia 14 Cavalase 38033
  Gemval s.n.c Instituto Analisi Gemologico Via Sassi, 44 Valenza 15048
Japan Association of Japan Gem Trust 2-3F Okachimachi Cy Bldg, 5-15-14 Ueno, Taito-ku Tokyo T110
  G.I.A 2-3F Okachimachi Cy Bldg, 5-15-14 Ueno, Taito-ku Tokyo T110
  Central Gem Laboratory Taiyo Bldg., 15-17,5-Chome, Veno,Taito-ku Tokyo 104
  Gemmological Association of All Japan Tokio-bihokaikan, 1-24 Akashi-cho, Chuo-ku Tokyo 104
Korea Mi-Jo Gem Study Institute, 244-39 Huan-dog Yongsan-Ku Seoul 140-190
  G.I.A KOREA Kangnamku Sinsadong 638-4, Kyung Jin Building-2nd Floor Seoul  
Netherlands Netherlands Gem Laboratory Hooglandse Kekgracht 17, 2312HS Leiden  
USA Holland School for Jewelers 231 Road St Box 882 Selam, AL 36701 Selam  
  International Gemological Services 4160 North Scottsdale Scottsdale AZ 85251
  Gemological Institute of America GIA The Robert Mouawad Campus 5345 Armada Drive Carlsbad CA 92008
  Gemological Institute of America GIA New York Campus
580 5th Avenue
New York NY 10036-4794
  Institute of Jewelry Training 3901 Northwood Av. Suite B Sacramento CA 90404
  Jewelry Technical Institute 1283 Western Ave. Garden Grove Garden Grove CA 90404
  Revere Academy of Jewelers Arts 760 Market # 939 San Francisco CA 90402
  American Society of Apraisers Box 17265 Washington DC 20041
  Keno Gemological Bureau 2000 E. Sunrise Blvd. Ft. Lauderdale FL 33304
  Art Institute of Atlanta 3376 Peachtree Rd. N.E. Atlanta GA 30326
  Atlanta Foundation for Jewlery Studies 110 E. Andrews Drive, #203 Atlanta GA 30305
  Emory University Evening at Emory Atlanta GA 30322
  Oglethorpe University 4484 Peachtree Rd. N.E. Atlanta GA 30319
  Parkland College 2400 W. Bradley Ave. Champaign IL 61820
  International Gemological School 3100 Ridgelake Drive Suite 301 Metairie LA 70002
  Columbia School of Gemology 8600 Fenton St. Silver Spring MD 20910
  Diamond Council of America 9140 Ward Parkway Kansas City MO 64114
  Fashion Institute of Technology 227 West 27th St. New York NY 10036
  Yeshiva University Midtown center 245 Lexington Ave. Lexington  
         




 

Birefringence

Birefringence is the difference in value between the highest and lowest refractive indices in a doubly refractive (anisotropic) material. Depending on the orientation of a faceted stone, this can result in a "fuzzy" appearance and apparent doubling of facets viewed through the stone.




 

Clarity

Gemstones can vary from complete opacity to lucid clarity and may contain few or many inclusions such as crystals of other minerals, gas- or liquid-filled cavities, or even insects! (Large, perfectly preserved insect specimens in amber are highly prized.) In some gemstones, such as emerald, certain inclusions are highly distinctive and can be used as reliable indicators of identity. A gemological microscope (a binocular microscope with a typical magnification of 10X to 40X) is one of the most useful tools in identifying many gemstones, as well as grading them on relative clarity.




 

Color

Color is the apparent result of selective absorption or transmission of different frequencies of visible light. Color can be described as the combination of three characteristics: hue, tone, and intensity. Hue is a function of the frequency of light and is described by familiar terms such as red, orange, yellow, blue, green, indigo, and violet. Tone is a variation from very light to very dark. Intensity is a measure of saturation, or purity, of a color. The typical human eye can identify approximately 150 pure hues, but around one million colors. The differences among colors may be immediately obvious or so subtle that direct comparison under controlled conditions is required to discern them. Color acuity is also highly affected by fatigue, diet, and other factors, so it is unwise to attempt judging subtle color differences in gemstones such as diamond without attention to the physical and emotional condition of the observer, as well as properly graded comparison stones and careful control of lighting conditions. 

Pleochroism is the apparent change in color of a doubly refractive gemstone when viewed through different directions of the crystal structure. In most cases, the color variations are not obvious to the unaided eye and must be viewed through a polariscope or dichroscope, but in some cases, the pleochroic colors are strikingly obvious. For example, many green tourmalines appear black through the C axis of the crystal, and iolite shows a striking combination of blue-violet and near colorless. Dichroism refers to the display of two ("di") pleochroic colors in a gemstone. 

Alexandrite-like color change, or photochroism, is the marked change in perceived color of a gemstone under different lighting conditions. As the name implies, the most famous example appears in alexandrite, a form of chrysoberyl that typically appears blue or green in daylight and red or purplish in incandescent light, but similar color changes may be observed in sapphire, garnet, and tourmaline. The phenomenon is due to selective absortion of different wavelengths of light, and the predominance or absence of those wavelengths in the prevailing light (incandescent light has proportionately higher quantities of reddish wavelengths and less of blue or green).




 

Dispersion

Dispersion is the ability of a gemstone to separate light into its component colors; that is, the quality of passing different wavelengths of light at different velocities. Dispersion is the quality in a diamond that produces sparkles of color in an otherwise colorless stone. Quartz, which has a dispersion of 0.013, shows much less of this effect than diamond, which has a dispersion of 0.044. Diamond, in turn, shows much less color play than sphalerite, which has a dispersion of 0.156.


 

Durability


The two most familiar qualities of durability -- hardness and toughness -- are often misunderstood. Hardness is resistance to scratching or piercing. Toughness is resistance to breakage. The combination of the two largely defines the durability of a gemstone. Diamond is the hardest naturally occurring material and is also quite tough; however, it can be broken by a hard blow. Jadeite and nephrite (the jades) are much softer and relatively easy to scratch but are perhaps the toughest gem materials. Hardness is often represented on the Mohs scale, a nonlinear scale of scratch resistance varying from 1 (talc) to 10 (diamond). The Mohs scale can be misleading -- there is a much greater difference in hardness between 9 (corundum) and 10 (diamond) than between 9 and 1 (talc). More precise, and less familiar, measurements of hardness are done using other systems, such as the Knoop scale of resistance to indentation. Because of the likelihood of physical damage, hardness tests are NOT recommended for gem identification. Resistance to chemical degradation or to changes in temperature or humidity are important. Turquoise is often quite porous and can be discolored by exposure to oils. Opals are heat-sensitive and have a high water content; sudden temperature changes or extremely dry conditions can cause them to crack or craze. 

Thermal conductivity (the ability to conduct heat) is very low in most gemstones but is extremely high in diamond (from 1.6 to 4.8 times as great as in pure silver!). This unusual property of diamond is the basis for several popular diagnostic probes that are used to distinguish diamond from its numerous imitations.




 

Fluorescence

Many materials are fluorescent. That is, when exposed to ultraviolet light or X-rays, they transform some of the incoming energy into visible light. The color and intensity of the fluorescence is often indicative, but not conclusive, of the identity of the material. For example, natural yellow sapphires from Ceylon show a distinctive apricot-colored fluorescence, while synthetic yellow sapphires generally show no fluorescence or a dull red when exposed to long-wave ultraviolet (UV) light. Most natural emeralds are inert (non-fluorescent) under long-wave UV, and most synthetic emeralds show a moderate to strong red fluorescence. Because of the prominent exceptions, this test alone is inconclusive.




 

Heat treatment

Many gems are routinely heated under controlled conditions to improve color (aquamarine, sapphire, ruby, tourmaline), alter color (sapphire, amethyst to citrine, topaz, zircon), or improve clarity (sapphire, ruby). Since natural heating also occurs (e.g., in volcanic areas), the artificial effects are sometimes indistinguishable from natural effects. In most cases, the results of heat treatment are permanent.




 

Impregnation and chemical treatment

Turquoise is often very porous and is sealed with wax or plastic resin to "stabilize" and improve the color. Such material is very abundant and often not disclosed. "Black onyx" is almost always agate that has been impregnated with sugar, which is then carbonized by acid. Yellowish diamonds are sometimes coated on the girdle or pavilion with a thin bluish film to improve color. Jadeite is sometimes chemically "bleached" and impregnated to improve color, and this treatment can be difficult to detect. 

In recent years, a new treatment for corundum has appeared, in which poorly colored corundum is heated in chemicals to deposit a thin (less than 0.5 mm) layer of enhanced color on the surface of the stone. These stones can be quite impressive, but recutting removes the surface coloration and results in a very disappointing stone. Such treatment is fairly easily detected by immersing the stone in a liquid with a high refractive index; the color appears to concentrate along facet edges. Until recently, only diffusion-treated blue sapphires were known, but the Fall 1995 issue of GIA's Gems and Gemology describes some diffusion-treated rubies, so other colors, and perhaps other stones, are likely to be entering the marketplace.





 

Irradiation

Colorless topaz is irradiated in large quantities and then heat treated to produce various shades of blue. Yellowish diamonds are often irradiated to produce a wide variety of colors. Other stones, such as tourmaline, are sometimes irradiated to enhance or produce new colors. In many cases, the effects of irradiation are somewhat unstable and can be reversed by heating.




 

Optic Character

Gemstones may affect the passage of light differently through different directions in the crystal structure. If the velocity of light is constant through all directions in the stone, the stone is said to be singly refractive, or isochroic, and has one refractive index. This is characteristic of isometric crystals. If the velocity of light varies with direction, the stone is doubly refractive, or anisotropic, and has two refractive indices. In anisotropic materials, light is separated into two polarized components, the ordinary ray and the extraordinary ray. Anisotropic materials can be further characterized as uniaxial, biaxial positive, and biaxial negative. 

Amorphous (non-crystalline) materials, such as opal, amber, and glass, may scatter light in unusual directions due to internal stress and display a phenomenon known as anomalous double refraction.




 

Phosphorescence

If a fluorescent material continues to emit light after the exciting UV or X-ray light is removed, it is said to be phosphorescent. This phenomenon usually lasts only a few seconds but may occasionally persist for much longer periods. This is a relatively rare characteristic in gemstones.




 

Refractive Index

Refractive index, or R.I., is the ratio of the velocity of light in air to the velocity of light through a transparent material. If light passes from air into a transparent material at an angle of incidence other than a 90 degree angle, it is deflected at a different angle (the coincident angle) according to the R.I. Gemstones with higher R.I. are generally more brilliant than those with low R.I. For example, diamond has an R.I. of about 2.4; quartz, about 1.54-1.55. The R.I. of most gemstones is easily measured using a simple optical instrument known as a refractometer.




 

Specific gravity

Gem materials vary greatly in density amber may float in salt water (density near that of water), while hematite is more than five times the density of water. This is why two different gemstones may have the same size but different weights and vice versa -- a one carat round brilliant diamond of typical proportions will be approximately 6.5 mm in diameter, while a round brilliant ruby of the same size (6.5 mm in diameter) and proportions will weigh approximately 1.55 carats. Generally, gemologists refer to specific gravity, or relative density the ratio of the density of a gemstone relative to that of water.





 

Gemstone treatment and enhancement

Gems are treated in different ways to improve their appearance. Some of these procedures are centuries old, while others are relatively new. Within the industry, these practices are taken as commonplace, while the gem buying public's awareness of these treatments has been much lower.
In this day of full disclosure and public awareness, the subject is coming to the forefront. Many industry officials are concerned that too much information will confuse customers and hurt sales. Others feel the public's right to know outweighs these concerns.
One certainly can confuse the public, as gem enhancement covers such difficult subjects as the physics of light response to molecular structure. However, some general comments are in order.

First, let me clarify that the term "natural gems" refers to those formed in the earth, whether or not they have been treated after mining. This, in contrast to "lab created," "man made" or "synthetic" gems.
The most common form of enhancement is heat treating. This is so common with corundum, (ruby and sapphire,) it is recommended that jewelers inform their customers that they are "probably heat treated."
"Probably?" That doesn't sound very professional. What is happening here is that the procedure so closely resembles what happens in nature, that one can't always tell if they have been treated after mining. Microscopic examination will sometimes reveal an inclusion that burst during heating, but lacking that there is no way to tell if the heat treatment was done before or after mining.
A similar situation occurs with aquamarine. If properly heated, it will lose it's green tint and become a pure blue. This is also identical to what happens in nature and there is no way of telling if it was done after mining. However, since most of the material coming out of the ground does have a green tint, it is recommended that the pure blue gems are described as "probably heat treated."
Very closely related to this is the treatment of blue topaz. Actually, it is a treatment of colorless topaz to turn them blue. This is done in two steps. First the rough is subjected to radiation to modify the sharing of electrons between certain atoms in the crystal structure. This turns the topaz brown. Then they are heated to become a stable blue color.
"Radiation!" Yes, this is one of the reason industry officials are reluctant to use full disclosure. Radiation is a scary word and telling someone a gem has exposed to it will certainly drive customers away.
However, this too exactly duplicates what happens in nature. Many gem crystals get exposed to radioactive elements during their formation. That doesn't mean they become radioactive, nor does it imply anything else. In fact, many gems seem to have beneficial effects on their wearers.

The above represent some of the most common examples of gem enhancement. The industry has never felt a need to disclose treatments that are indistinguishable from the processes that occur in natural formation. However, there is one other common enhancement that falls into an entirely different category. That is the oiling of stones.
Some gems, most notably emeralds, have internal fractures. Light reflects off of their surfaces, which seriously effects the clarity and brilliance of the gem. However, by simply filling them with a substance of similar optical properties, the tiny cavities once again become transparent. The difference in the appearance of the finished gem can often be startling!
Now, how chicken this is depends on your point of view. To the gem cutter, this is a serious problem. Those tiny fractures represent areas of weakness that have to be considered in the cutting process. If masked with oil, the risk of damage during cutting becomes much greater.
To the proud owner of an emerald, the improvement to it's appearance is well worth it. One doesn't see the oil, it simply allows the natural beauty of the gemstone to stand out. Both the emotional and the monetary value of the gem are considerably enhanced.
However, the owner should certainly be made aware that it needs special care. Continual washing of dishes while wearing an emerald ring can cause it to lose its brilliance. Vigorous cleaning methods, like using heat or immersing in an ultrasonic jewelry cleaner can be disastrous.

There are many other ways gems can be enhanced. Inexpensive ones are often dyed, the porosity of turquoise is often sealed so body oils don't discolor them, etc. However, the above represent the most common examples one is likely to come across. More detailed information will be available in the "Advanced Gemology" section.




 

Hardness

The power a stone possesses to resist abrasion when a pointed fragment of another substance is drawn across its smooth surface without sufficient pressure to develop cleavage (GA course material).

Harder stones will scratch softer ones. Stones of the same hardness may scratch each other (a diamond can scratch a diamond). The Mohs scale is used for gemstone hardnesses. This scale is purely relative as shown by the fact that the difference in hardness between corundum (9) and diamond (10) is 140 times the difference between talc (1) and corundum (9).

Mohs Scale
1. Talc
2. Gypsum
3. Calcite
4. Fluorite
5. Apatite
6. Orthoclase feldspar
7. Quartz
8. Topaz
9. Corundum
10. Diamond

Other reference points include:
Finger nail 2 1/2
Copper penny 3 or so
Window glass 5 1/2 or so
Knife blade 6
Steel file 6 1/2 - 7
Silicon carbide 9 1/4
Carborundum 9 1/4

Hardness testing is not often used as the chance of damaging a good stone or even an imitation of value to the owner is too high. It is normally only used on rough material or on an inconspicuous spot on large carvings as a confirmatory test.

Any scratch detracts from the value of a gem. It will not tell if something is synthetic or natural.

Hardness points Sets of standard pieces of Mohs hardness 7, 8, 9, 10 mounted in rods used to scratch gem materials.

Hardness Plates Sheets or slabs of standard hardness materials. The gem to be tested is rubbed on the plate using the girdle so that hopefully the plate suffers the damage. Again, material can scratch itself although it is true that the feel of the bite in hardness testing can tell a great deal.

It is also not necessary to file chunks from gems or scratch whole facets; a 1 mm scratch can suffice and if the plate and stone is wiped clean and inspected with a loupe one can tell which was scratched. Diamond is the only colourless gemstone which will produce a scratch in a polished corundum plate.

A lapidary can make a set of small plates quite easily and synthetic corundum can supply the #9 plate.




 

An Introduction to Gemology

Gemology is the study of gemstones. Some dictionaries define it as the "scientific study of gemstones," but it is almost impossible to remove the scientific element. There may be investors whose only interest is in the value of the stones, but if they ever need to distinguish one gem from another, they are dealing with science.
There are many categories of gemologists. For the jeweler it is a key element of their business. They need to be able to answer their customer's questions and identify the gems brought into them.
The gold smith needs specific knowledge about the physical characteristics of gems. A setting that would be ideal for a diamond would be inappropriate for an opal and vice versa. The amount of pressure used to set the prongs on a garnet would break a tanzanite.
Some gems will withstand the heat of repair work that involves high temperature soldering. Some can be left in the setting if steps are taken to moderate the amount of heat they receive. Still others are so heat sensitive they need to be removed.
The lapidary also needs special knowledge. Cutting and polishing techniques vary from gem to gem. What would work well for one material would be a waste of time on another and disastrous on something else.
When faceting thought needs to be given to color management. How the rough is oriented can make a lot of difference in the appearance of the finished gem. The style of cutting is also a part of color management. The choice of cut can lighten or darken a gem which will have considerable effect in both the appearance and the value of the stone.
The choice of a cut, which includes the shape, number and location of facets, also influences the brilliance of the gem. The angles the facets are cut at have to be carefully chosen. Then these factors are balanced, or compromises made, so as to not sacrifice too much material in the pursuit of beauty.
Another category of gemologist are the scientists. These are people with degrees in geology, chemistry and sometimes physics. While one of the smallest categories of gemologists, they are at the same time one of the most influential.
At the heart of gemology is gem identification. Some rubies and garnets are impossible to tell apart from each other by observation, but their values are considerably different. A precise and accurate means to tell them apart is absolutely necessary.
When dealing with whole crystals, the ruby and garnet are easy to distinguish. Garnets form in the cubic system. While they vary in shape, they tend to be roundish and the number of sides is always a multiple of four. Rubies on the other hand, form long thin crystals. They are in the hexagonal system and always have six sides.
Most of the material that gets cut into gems isn't found in whole crystals, but in broken pieces. Using the techniques of mineralogy, they are easily distinguished from each other. Scratch tests, where the unknown is scratched by various substances, will determine its hardness. Other useful tests are the reaction to acids and the flame of a blow torch. These are categorized as destructive tests and are obviously inappropriate for cut gems.
For centuries it was the lapidary who was in a position to most easily recognize the differences in like appearing gems. During the cutting process gems get viewed intently, a perspective that no other gemologist has. Identifying inclusions are given a lot of attention, then as many as possible removed. Differences in hardness are readily apparent when cutting and polishing, as are other characteristics.
A method needed to be devised where cut gems could be identified without damage. To this end scientists began to first, identify the measurable physical and optical properties of our gems. Next they devised instruments to measure these properties. There was a long process of systematically measuring and recording these properties so they could be looked up. (Though well established, this is actually an ongoing process.) Eventually all this got put together into methods that could be used by people without extensive scientific backgrounds or large and expensive laboratory equipment.
That is not to say that it doesn't require substantial education to identify gems. It is a large and complex subject that is continuing to increase in complexity as new gems are discovered and new ones are created in the laboratory. However, one doesn't need a degree in chemistry or physics to simply measure the properties of our gems. The most esoteric part was discovering those properties and creating the tools to measure them.
If you are interested in learning about gems the first step would be to learn how they are categorized. Also important in the early stages is learning the terminology used to describe gems. Next you can learn what the physical and optical properties are. When you have this background, you can get into gem identification.
Of course there are many side roads to travel. You may find a fascination with phenomenal gems or their inclusions. Many people find a desire to collect gems and this often leads to making jewelry or learning how to cut gems.
Whether your interest is casual or professional, there is much to delight and amaze. It is something you can do from your desk, or something that allows you to get your hands dirty. Plus the subject of gemology is one of those where you will never run out of new elements to discover.




 
LAP MATERIAL

MOH'S

COMMENTS
Ceramic

9

Aluminum Oxide
Anodized Aluminum

6.5

Electrolytic coat
Steel

5 to 8.5

.
Cast Iron

5

.
Corian

4

Methal methacrylate plastic
Copper

3

.
Zink

2.5

.
Plexiglass, Lucite

2

Acrylic Plastic
Type Metal

2

Lead, tin, antimony, copper
Pewter

2

Lead, tin and variables
Metallized Resin

1.9

Metal pelets in resin
Type Metal

1.8

Tin and variables
Tin

1.7

.
Mylar

1.6

Polyester plastic
Acetate

1.6

.
Lead

1.5

.
Polyurithane

1.5

.
Vinyl

1

.
Beeswax/carnuba

0.3

.
Beeswax

0.2

.

 




 

Some Notes on making your own polariscope for gemology

Polariscopes are a very useful, simple and inexpensive to make piece of gemological equipment. They are used to tell glass from gem materials synthetic spinel from all other materials, singly refractive from doubly refractive, crystaline from cryptocrystaline material, doublets and triplets from other gems, identify yellow Verneuil corundum (Plato test-see Liddicoat -GIA), determine quartz definitively from other materials, tell whether a transparent gemstone is biaxial or uniaxial in its crystal system. This is pretty good or equipment that may be as simple as a camera lens and a pair of polaroid® sunglasses.

This is one piece of gemological equipment that is fairly expensive and can be made very easily and cheaply. Prices for polariscopes start around $65.00 and go up. Hanneman has a very basic model (two sheets of polaroid and a tube) for around $4.00 and supplies two 2" x 2" sheets of polaroid filter material for $1.00. I have made one using two polaroid sunglass lenses on a stick and a student I had (Dennis O'Hanley) used sunglasse lenses and an empty underarm deodorant tube container with holes cut in top and bottom to fit the lenses. He cut an access port in the side to permit manipulation of the gemstone (1.3). One could rotate the top of the deodorant tube to cross the filters as needed. My own polariscope was made using two 49mm camera polarizing filters ($14.00 total) and a length of appropriately sized PVC pipe. Two rings were cut off the end of the pipe, small segments cut out of these rings so that they could be forced together and slid into the pipe where they formed ledges upon which the camera filter sit. An access port was then cut in the side of the PVC pipe. An advantage of using commercial lenses is that they rotate freely when in place. The GIA microscope immersion cell (about $10.0) just fits in the filter (49 mm) so that several gems at once may be examined in polarized light conditions by rotating the immersion cell. It is made in such a way that the glass of the immersion cell does not interfere with polariscope use.

Illustartion 1

A light source would be a flashlight, which fits in the tube also. I use my microprojector as a light source. A paper disc is placed just below the lower polarizing filter to diffuse the light somewhat. A strainless glass sphere on a rod is available for resolving interference figures of gems with the polariscope. This would identify quartz and tell whether a gem is biaxial or uniaxial in crystal system. GIA and Hanneman sell them.

Mr. Hamilton Stitt, F.G.A. described a very simple field polariscope in the Journal of Gemmology. A polaroid filter is placed over the glass in the well of a small flashlight. One then dons polaroid sunglasses and has an instant polariscope with an adjustable distance between lower (flashlight well) and upper (sunglasses) filters to examine stones. The rim of the flashlight prevents stone loss and interference figures may be resolved with a 10X hand lens. This is really a pocket polariscope.

Using the polariscope
To use the polariscope the top polarizing filter is turned to the extinction position (dark) allowing the least amount of light to pass through the two filters. The stone is placed between the two filters and rotated around a vertical axis. If it darkens evenly at exactly 90o intervals (4x per rotation) it indicates double refraction. It is important to test each stone in more than two positions as a doubly refractive stone may have one or two directions of single refraction (optic axes) in it. If it remains dark throughout its rotation single refraction is indicated. Cryptocrystalline material remains bright during rotation (jade, chalcedony) but some glass with textured backs does the same so it is best to use this test for transparent stones only. Note that large numbers of doubly refractive inclusions would have a similar effect. Brilliant cut stones should not be tested table up or down as they may reflect out all the light entering the table giving a false reading.

Anomalous double refraction may occur in singly refractive materials with internal strains such as diamond, garnet, synthetic spinel, amber, plastic, opal and glass. The extinction patterns here however do not occur at precisely 90o intervals although rarely they may be close. Plastic and amber may show bright interference colours. Glass may show a characteristic cross like shadow, or two approaching bars which almost form a cross during rotation. Synthetic spinel shows a characteristic 'tabby' extinction, a sort of fine, mottled cross hatching of parallel silk-like lines which change during rotation. In a doubly refractive stone interference colours will appear when one is within a few degrees of an optic axis. To produce diagnostic interference figures one obtains the optic axis position and placed a condensing lens above the stone or in contact with it. This can be a 10X lens (viewed from 18" or so distance), a drop of viscous liquid or a strainless glass sphere. This will divulge whether the stone is uniaxial or biaxial.

The characteristic interference figure for uniaxial gems is:

Illustration 2

Quartz has a special variety of this uniaxial figure called a bullseye uniaxial figure and this is, if seen clearly, diagnostic for quartz. The centre circle is often red.

Illustration 3

Biaxial figures vary somewhat but are quite distinctive having usually only two arms or brushes from a centre or oval:

Illustration 4

It may be noted that cabachon gems or beads often need no condensing lens as they function as one themselves. Interference figures may be resolved more easily if the gem is immersed in water or bromoform (toxic). Be sure that the transparent container for your liquid does not itself add shadow lines to your image, especially if merely testing for double refraction. Interference figures may be used to distinguish between: moonstone (orthoclase) and chalcedonic quartz which shows no figure resolution, topaz and tourmaline, andalusite and tourmaline, corundum and chrysoberyl.




 

The microscope


To view inclusions, a microscope is required. In terms of optics, look for a stereo-zoom head with a magnification range from 10-60x (this can be increased with stronger eyepieces and/or a doubling objective lens). Surprisingly enough, quality of optics is not nearly so important as the microscope base. Many so-called gemological microscopes are lacking in one important area – lighting. Without proper illumination, one sees nothing, even with the best optics. Thus a microscope must possess an extremely strong, built-in light source (a 35-watt quartz halogen bulb is the absolute minimum).

GIA/Gem Instruments' Gemolite base is one of the best available for all-round use. Even better is that designed by Marc Bogerd and the author for the Asian Institute of Gemological Sciences.
The Gemolite is greatly improved by modification. Dump the 35-watt bulb and move up to a more powerful model. Use of a bulb with a vertical filament (as opposed to horizontal) produces a wider band of effective illumination. While the stronger bulb may create problems for heat-sensitive gems, it is worth the risk. Once again, if the specimen is not adequately illuminated, you see nothing.

The humble stoneholder is another oft-overlooked aspect of microscope design. A poor-quality stoneholder inevitably results in the "jewelers' prayer meeting" – down on your knees praying to find a stone that has flown out of sight. Surprisingly, many stone holders lack a knurled groove on the inside to grasp the stone's girdle. The best used by the author was that made by GIA/Gem Instruments; however it is no longer made.




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