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Gemology
Gemology is by definition the study or the science of
precious stones. One knows approximately 4000 minerals
produced by the terrestrial body, among which less than 100 produce specimens considered as precious stones. To be a gem, a mineral must have three fundamental virtues. Beauty, durability and scarcity.

Beauty; it depends on the following characters:

Transparent minerals: The glare (brightness) dispersion (fire) the transparency (purity) intensity of the color (for the colored stones)

Translucent minerals : 

Color or reflection, opalescence, changing luster or asterism (in the case of the phenomenal stones)

Opaque minerals:

Purity and intensity of the color, the propensity to well  reflecting their color and taking the polish. All these factors of beauty are highlighted by the size and polishing.

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           Andranondambo Sapphire Discovery
        The story
Durability depends on resistance to the mechanical or chemical attacks to which the stones are subjected. Dust often containing quartz particles. It is preferable that a gem is as hard as this mineral.

Rarity: A gem often comes from a common and very widespread mineral species, but it consists of a specimen in which exist seldom joined together qualities.

Gemology is the study of significant properties of the gems, it serves of the apparatuses or instruments necessary to the observation and the measurement of these properties.

The gemologist must be able to differentiate the natural stones from the synthetic stones using his instruments.

- Here are the principal instruments used by the gemologist:
The eye which will transmit to the brain the visual data processed instantaneously by the data base in it containing the more or less large experiment of the gem's observer.

The  loupe"10x" It is under this enlarging that, by International Convention, the

purity of the stones must be given. Especially diamond. The strong curve of the

lenses used for the loupe "10x" has as a corollary a considerable marginal distortion

and chromatic aberrations, unless the loupe is made up of a whole of lenses

calculated to eliminate these disadvantages. An anastigmatic loupe of good

quality is significant for the gemologist.

The preliminary examination at the eye then with the loupe "10x" is thus of primary importance 

because the characteristic signs of a gem will help the gemologist to choose effective instruments 

for the identification.

- The characteristic signs of a gem which one can observe to the naked eye or with the loupe are as follows:

Texture: rough gem or opaque

Gloss: diamantine, vitreous or resinous etc. 

Substantial dispersion (indication of a high index of refraction) or weak, presence or absence of cleavages.

Characteristic fracture: vitreous, granulous or splintering etc.

Assembled stone: doublet or triplet.

 

Corners between the facets: sharp or round, often with the concave facets (indication of glass or a cast plastic) or notched (stone of low hardness).

Abundant inclusions: which make the gems translucent, and by consequence, the optical signs could not be obtained under the polariscope.

Moreover, one could not insist enough on the importance of a perfect cleanliness of the stones to 
examine.  The cleaning of the unset stones is easy;  it is enough to wipe them with a clean
handkerchief.  A good cleaning can be obtained with water accompanied by a little liquid
detergent.  
To avoid dirtying the stones,  the specialized tweezers represent a pleasant complement to the 
fingers.
- Scale determining the purity of a stone.  -
FL NFL SI1 SI2 MI1
Flaw less Near flaw less Slightly included 1 Slightly included 2 Medium included 1
-------------------------------------------------------------------------------------------------------------------------------------------------------------------
MI2 MI3 VI1 VI2 HI
Medium included 2 Medium included 3 Very included 1 Very included 2 Highly included
   Note that our camera can grasp very small inclusions almost invisible to the naked eye;
       this is why you can usually see these inclusions on the screen.
The Polariscope, here a pocket polariscope.
It is the usual means by which one differentiates on the one hand
the unirefractives substances  (amorphous or coming from the cubic
system) and the birefractives substances, coming from the other
systems of crystallization.
This instrument is composed of two filters polarizing between which
the stone is placed, and it is while turning the filter of the top that
the analysis can be done.
The refractometer is used to determine the indexes of refraction 
of the stone. This instrument calculates speed with which luminous
rays arise from the stone and indicates it on a scale.  The gem is
placed on a coated pane of a fine particle of liquid made up amongst
other things of methylene iodide which shows an index of refraction
of 1.81 (this liquid is toxic)
Dichroscope of which the principal part is made up of a tube 
comprising a window with the one of the ends and a lens with the 
other, between the two is assembled a piece of calcite, chosen 
because of its strong double refraction so that two images of the 
window appear side by side to the observer which looks in the 
eye-glass.  The light of the adjacent images of the window vibrates 
in two perpendicular plans one to the other at a rate of one only plan 
for each image.  The rotation of the stone is a significant factor 
during the control of dichroism, bus in all the double refraction 
stones, it exists one or two directions of unirefringence, known as 
optical axe.
The Chelsea color filter. There is a very effective means to
reveal the subjacent differences in color, it is the use of colored
filters.
They are especially effective in the differentiation of natural and
synthetic emerald. 
The optical fiber lamp is useful to distinguish inclusions in rough
stones. 
Microscopes:  the binocular one, i.e. to double objective is best
adapted for gemology.  The microscope is of first importance in 
the detection of counterfeits.  Indeed, the study of inclusions
which the stone can contain is a practical means to identify the 
gems while explaining to a certain extent the conditions under which 
they were formed in nature.
    
Malaya garnet discovery
 

The spectroscope concerns an extremely simple method which
allow the identification of all the stones; rough or polished not being
able to be seen with the refractometer and which even makes it
possible to distinguish certain synthetic or glasses.  This method
makes it possible to analyze the nature of the dye of the stone. The
way in which the spectroscope analyzes the various wavelengths of
the light is in theory very simple;  that depends on the different
degree of refraction to which its subjected various rays of each color
(wavelength) when they are propagated through a prism of glass or
another transparent substance.  After having passed through a
prism, a narrow parallel beam of white light is spread out in a ribbon
with the colors of the rainbow, the visible spectrum.
Let us note that a powerful instrument used in many fields of science
is at disposal of the gemologists, it is the microscope of Raman which
spectroscopy supplements the traditional technology of the
laboratory.  This instrument can give information on samples lower
than 1m what is not accessible to any technique.  The use of the
Raman spectroscopy by imagery is unique in order to determine in a
nondestructive way the molecular composition of inclusions present
in the gems.
Analyze by fluorescence:  four kinds of radiation are used.
The first consists simply in passing a powerful luminous ray of a lamp of projection of 500W through a balloon filled with a strong copper sulfate solution, this last absorbs all the red light, orange and yellow and the filter rays are invisible if one observes through a good red or orange filter.  If a substance only lit by the beam of blue light in which it is shines while being observed through one of these filters, it emits a fluorescence.

The second method of stimulation of fluorescence is the used, it uses a lamp with high pressure out of quartz, and whose light is filtered through the glass of Wood.

The third uses the ultraviolet radiations of short radiation emitted by a quartz-mercury lamp with low pressure, in which the mercury line with 2537 is dominating.

X-rays represent the fourth source of radiation, they are dangerous unless the source is not seriously armored.

The unit weight and its measurement.  It frequently occurs that only an approximate value of
the density of a stone is necessary to differentiate between gems from similar appearance; in this
case a control from the density can be carried out by means of liquors of density.  The principle of
the method is simple.  A stone will be inserted in a less dense liquid, will float in a denser fluid and
will remains in suspension in a liquid of equal density.
The three liquids are:
The bromoforme density 2,9.
The methylene iodide density 3,33.

The liquor of Clerici density 4,15.

PRINCIPAL COLORING ELEMENTS IN THE GEMS.
            Chromium   Ruby, EmeraldPyrope garnet, grossularite and uvarovite, Tourmaline.
            Copper   Dioptase, Malachite, Azurite.
            Iron   Sapphire, Aquamarine, CitrineAlmandin garnet.
            Manganese   Morganite, Pink tourmaline, Spessartite garnet.
            Nickel   Chrysoprase.
            Titanium   Blue Sapphire.
            Vanadium   Green beryl, Blue zosite , Garnet.
 
    Cutting Styles Fancy Cutting  Characteristics Crystalline Systems Size & Weight  
 
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All of the pictures on this website have been shot by gggems.com
Text written by Alain Darbellay.
 
 
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