How to Value a Diamond:

 

When considering purchasing a commodity as precious as diamonds, it is important to know the factors affecting the true value of a given stone. Most "Jewelers" will promote carat weight as the primary determination of value when, in fact, cut, color and clarity can all have greater influence on the value of a loose diamond than carat weight alone.

 

The Gemological Institute of America (GIA) has taken great strides in developing a grading system to standardize value in diamonds. These diamond-grading standards are applied to cut, color and clarity by professionally trained gemologists worldwide. Having noted that, it is also important to point out that there are other International or universal grading systems that are as effective and almost as wildly used as the GIA grading system. The basic 4 Cs that is used in determining the value of a diamond are as follows:

 

1. Carat Weight

 

Carat is often confused with size even though it is actually a measure of weight. One carat is equivalent to 200 milligrams. One Carat can also be divided into 100 points. A 0.75-carat diamond is the same as 75 points or a 3/4-carat diamond. Larger diamonds are found relatively infrequently in nature and are therefore more valuable.

Please note that a 1-carat diamond doesn’t cost exactly as 2 (0.5 carat) diamonds. Since the larger diamonds are found less frequently in nature, a 1-carat diamond is much more expensive than twice as much as a 0.5 carat diamond. Assuming cut, color and clarity remain constant.

 

The word Carat is derivative of the world carob. Carob sees are surprisingly similar in weight to one another; thus, they were used in ancient times as the reference tool to measure the weight of a diamond. One carob seed equaled 1-carat. Please also note that carat (“ct”) is not Karat (Kt) which refers to the purity of gold.

 

2. Cut

 

Just like water, glass or any other transparent medium, the density of diamond will "bend" light at a specific angle as it passes through.  In the 18th century, a mathematician named Marcel Tolkowski developed a mathematical model that calculated the behavior of light as it passed through a diamond. He used this model to determine the optimum angles of cut that would reflect and refract the greatest amount of light back out the top of a diamond. These "Ideal" proportions are alternately referred to as "Tolkowski Cut", "GIA Class 1 Cut" and "AGS 0 Cut". True "Ideal" proportions have only been calculated for Round Brilliant Cuts. They are listed in the Table and Depth Percentage Chart below, as well as the best or "preferred" cut proportions for the other shapes.

 

Table and Depth Percentage are two critical measurements for loose diamonds. The angles of cut will affect a diamond's natural ability to both reflect and refract light, that is, the diamond's ability to virtually explode with brilliance. If a diamond is cut too deep, light leaks out the sides, brilliance is lost and the center of the diamond will appear to be dark. If a diamond is cut too shallow, light leaks out the bottom and the diamond appears watery, glassy and dark. If the proportions are good, the sides and bottom of the diamond will all reflect their light back out to the top of the diamond, which creates the brilliance diamonds are famous for.

The Table percent is the width of the top facet of the crown compared to the diamond's total width. Table width between 53% and 64% are considered Preferred in Round Brilliant Cut diamonds.

 

The Depth percent is the total depth or height of the diamond compared to the total width. Depth measurements between 58% and 63% are considered Preferred in Round Brilliant Cut Diamonds. The Preferred range for these measurements will change as the shape changes, i.e. a Marquise cut diamond will have different ranges for Premium Table and Depth percentages. The following table shows the Ideal ranges for depth and table for Round Brilliant diamonds as well as the Preferred ranges for Rounds and all other shapes:

 

Table and Depth Percentage Chart:

IDEAL SHAPE

DEPTH RANGE

TABLE RANGE

Round Brilliant

59% to 62.6%

53% to 57%

PREFERRED CUTS

 

 

Round Brilliant

58% to 63%

53% to 64%

Marquise, Oval, Pear

58% to 66%

56% to 64%

Emerald, Radiant

59% to 69%

60% to 69%

Princess

60% to 75%

60% to 79%

Heart Shape

55% to 65%

51% to 65%

 

Naturally, diamonds with measurements within those ranges will be more expensive than diamonds with measurements outside those ranges. You need to balance that decision yourself. A few %'s one way or the other are minimal.

 

Besides Table and Depth Percentages, there are several other minor grading factors that combine to affect the diamond's beauty and value.

 

Polish measures the quality of finish on the facets.

Symmetry refers to the proper alignment of the diamond's sections, the proper shape for the cut (circular for round brilliants, rectangular for emerald, etc.) and the uniformity in size and angles of similar facets.

Both Polish and Symmetry are rated as: Excellent (EX), Very Good (VG), Good to Very Good (GVG), Good (G), Fair to Good (FG), Fair (F), Fair to Poor (FP), or Poor (P). An excellent rating is very rare. The Very Good, Good to Very Good, and Good ratings are common and desirable. They will also affect the price, though not as much as Table and Depth.

Fluorescence, normally blue, can naturally occur in diamonds and becomes visible under Ultra Violet light. Fluorescence can be clear or cloudy. Cloudy Fluorescence is undesirable. Fluorescence can be rated as: Nil or None, Very Faint, Faint, Medium, or Strong. Nil to Faint Fluorescence will have negligible impact on a diamond. Medium to Strong Blue Fluorescence can actually be an asset in Color Grades I, J, K, L and up as it will tend to enhance the diamond's brilliance and make it appear "whiter".

 

The Girdle is the spacing between the upper and lower portions of the stone. Girdles can be rated from extremely thin to extremely thick. Extreme grading should be avoided. The girdle finish can be natural, polished of faceted. Finer diamonds will normally have faceted girdles.

The Culet size refers to the smallest polished facet at the very bottom of the diamond. Avoid large or chipped culets. 

 

Unfortunately, these ideal cut diamond proportions require a great amount of the diamond to be cut away, minimizing the remaining carat weight. Since loose diamonds are priced and sold by carat weight, this creates a natural contradiction in priorities: cut quality or carat weight? A properly cut diamond will virtually explode with dazzling brilliance and color. An improper cut, often for the sole purpose of leaving added carat weight, will leave dark, glassy or watery looking areas in the diamond. Less than 10% of all Round Brilliant diamonds qualify for true Ideal Cut, and only about 20% of all loose diamonds qualify as Preferred Cut. That leaves 80% of the market cut with carat weight as the priority as opposed to brilliance.

 

 

Diamond Cutting Tools and Machines

 

 

        

 

 

3. COLOR

Diamonds vary in color from colorless to slight tones of yellow or brown. Colorless diamonds are most brilliant, most rare and most valuable. The following scale shows the GIA loose diamond color rating systems. The D-J ratings are among the most desirable.

           

Color Chart

Colorless

Near Colorless

Faint Yellow

Very Light Yellow

Light Yellow

D E F

G H I J

K L M

N O P Q R

S T U V W X Y Z

 

   

 

Truly colorless diamonds such as D are extremely rare and consequently extremely valuable.

 

4. CLARITY

Practically all diamonds contain naturally occurring internal characteristics called inclusions. The size, nature, location and number of inclusions determine a diamond's clarity grade and affect its value. 

The following scale shows the GIA diamond clarity grading:

 

Clarity Chart

FL

IF

VVS1 - VVS2

VS1 - VS2

SI1 - SI2

I1 - I2 - I3

Flawless

Internally Flawless

Very Very Small

Inclusions

Very Small Inclusions

Small Inclusions

Imperfect

 

 

FL:                  Flawless -- no internal or external inclusions of any kind visible under 10x magnification to a trained eye, the most rare and expensive of all clarity grades

 

IF:                   Internally Flawless -- no internal inclusions visible under 10x magnification to a trained eye, but there may be some tiny external irregularities in the finish

 

VVS-1:            Very Very Slightly Included 1 -- usually just one tiny inclusion visible only to a trained eye under 10x magnification

 

VVS-2:           Very Very Slightly Included 2 -- tiny inclusions visible only to a trained eye under 10x magnification

 

VS-1:              Very Slightly Included 1 -- very small inclusions visible with 10x magnification

 

VS-2:              Very Slightly Included 2 -- several very small inclusions visible with 10x magnification

 

SI-1:               Slightly Included 1 -- small inclusions visible with 10x magnification

 

SI-2:               Slightly Included 2 -- several small inclusions visible with 10x magnification

 

SI-3:               Slightly Included 3 -- inclusions that may be visible to the naked eye for a trained observer

           

I-1:                  Included 1 -- flaws that are visible to the naked eye

 

I-2:                  Included 2 -- many flaws clearly visible to the naked eye that also decrease the brilliance

 

I-3:                  Included 3 -- many flaws clearly visible to the naked eye which decrease the brilliance and compromise the structure of the diamond, making it more easily cracked or chipped

 

NOTE: We feel that diamonds of clarity grades I-1, I-2 or I-3 (Imperfect 2 and Imperfect 3 as described by GIA) are not ideal as a representation of the bond of eternal love. Therefore, we do not recommend diamonds of these clarity grades for engagement rings. We can provide you such diamonds upon request only.

 

Additional Information about Diamond

 

Diamond Properties

 

Technical Information:  

Colors:                                                Colorless, Yellow, Orange, Brown, and Black.

Extremely rare colors:                       Red, Blue, Green, and Purple.

Chemical composition:                    C - carbon

Crystal Structure:                               Cubic - isometric

Hardness:                                          10

Specific Gravity:                                3.52

Note:                                                   Size is relative to specific gravity, its density. A 1.00ct opal would be much larger than a 1.00ct diamond. A 6.5mm sapphire of equal cut would be 1.14ct.

Refractive Index:                                2.42 - singly refractive.

Dispersion:                                        .044

Fluorescence:                                    Photoluminescence - A natural occurrence of some diamonds, the emission of a visible glow stimulated by invisible wavelengths, UV light. Diamonds can fluoresce any color; the most common color is blue.

 

 

 

The strength of fluorescence is described in the following terms:

 

None: also known as inert.

Faint: occurs around the girdle's edge 

Moderate: glows, but not strongly 

Strong: the whole stone glows brightly

 

Other Varieties:                                 Bort

Poorly Crystallized,

Inferior color.

Carbon ado

Gray to black to opaque in color.

Used as abrasives in cutting diamonds, and bits for drilling rock.

 

 

Scientists have divided diamonds into 2 groups:

Type I - gem quality stones are characterized by their absorption of the ultra-violet below about 3000A and by an absorption band in the infrared.

Type II - transmit ultra-violet to about 2250A, and this group is further divided into 2 sub-groups Type II a, Type II b. The latter being the interesting as natural blue-colored stones and is electro-conducting.

 

 

THE SCIENCE:

 

Diamonds are the crystalline of carbon, transformed by extreme heat and pressure. There is only one natural environment in which diamonds can be formed, and that is in molten rock from 75 to 120 miles below the earth's surface.

 

Diamond crystals then surface in volcanic eruptions. The trip is precarious: the crystals may revert to free carbon atoms, vaporize into carbon dioxide, or turn into graphite (the common "lead" pencil ingredient) along the way. The only way diamond preserves its original form is through a rapid cool-down near the earth's surface. With a few unusual exceptions, the only kind of rock that can bear diamond to an accessible depth is called kimberlite, after the town of Kimberly, South Africa. Kimberlite surges up through the earth in carrot-shaped cones known as "pipes." There are few kimberlite pipes in existence, and not many contain important quantities of diamond.

 

Diamonds form under large, stable, cooler plates of earth called "cratons." Dry earth diamond sites are known as "primary deposits" because they lead directly down to the stones' subterranean birthplace. But it is only since the South African diamond rush in the l870's that diamonds have been mined from dry earth -- for thousands of years diamonds were only sought in riverbed sands and gravel.

Alluvial diamond sites are called secondary deposits. Massive geological shifts, and the movement of glaciers and water can bear diamonds thousands of miles from their original underground source. Most of the world's finest diamonds were discovered in secondary deposits, in the famous riverbed mines of India.

Diamonds can also travel to marine deposits. At present, one of the richest of the world's diamond sources is found on a l00-mile stretch of beach south of Namibia. Eons ago these were South African diamonds, carried downriver in dirt and gravel debris toward the Atlantic Ocean. The larger diamonds sank into the ocean floor, while others were left at the shoreline by currents and storms. It is thought that Antarctica may be a rich potential source of diamonds. However, international accords prohibit mining Antarctica.

 

 

Be Aware Of Diamond Treatments:

 

Yes, it is true, diamond can be treated and the following is provided for your

Information:

 

Diamond Treatments

 

Some treatments can provide a solution to the problems of a diamond, making it more valuable. Your jeweler should disclose any treatments or enhancements, ask if the diamond you are considering is treated. Most reputable jewelers will disclose this fact.

 

Clarity Enhanced, Fracture Filled Diamonds

 

The clarity enhancement process was developed in 1982 by Israeli inventor and diamond cutter Zvi Yehuda, and involves filling cracks in diamonds with molten glass to improve their clarity. Only diamonds with small cracks can be treated, and this method improves diamonds clarity by one grade without affecting the color or weight of the diamond.

 

Not all clarity-enhanced diamonds are the same, nor do they all come with a guarantee. Some companies use bromine to enhance their diamonds because the process is cheaper than using glass. Diamonds treated with bromine have been known to discolor and cloud with exposure to the ultra violet radiation found in sunlight.

 

Laser Drill

 

Since the 1970's lasers have been used to burn minute holes in diamonds to reach dark inclusions and bleach them with acid so they are less visible. Some are then filled with a glass like substance.

 

Irradiated Diamonds

 

The affordable Fancy colored diamond. Artificially colored by electron bombardment. The coloration is permanent.

 

Painted for color

 

Diamond can be painted to offset a yellow tinge.

 

Coated Diamonds

 

Some diamonds are coated to enhance or improve their color. A coated diamond might go undetected for years if the diamond is not examined by an experienced grader, gemologist.

 

If you decide to buy a diamond that has been treated, and later that item needs to be cleaned or repaired be sure you disclose the type of diamond treatment to your jeweler to avoid any damage to your jewelry or misunderstandings. Find out more about treated diamonds to help you decide if this is a choice you really want to make.

 

Notice:

We do not sell, or deal with diamonds that have had any of the above red treatments, or any treatment at all. 

 


 

Diamond Look a Likes:

 

            The following may have the appearance of natural diamonds, but do not share the same physical, optical and chemical properties. The most common simulates include colorless glass, white sapphire, white topaz, synthetic cubic zirconia and, synthetic moissanite.

 

Info:

Diamond

Simulate

Types

Synthetic

Cubic Zirconia

Synthetic

Moissanite

Real

Diamond

Hardness:

81⁄2

91⁄4

10

Toughness:

Good

Excellent

Good

Specific Gravity:

5.65 - 5.98    

3.21   

3.52

Dispersion:

0.060

0.104

0.044

 

 

CZ is actually the better diamond simulate even though it is softer than Moissanite. Both of these stones can not compare to diamonds natural inherent beauty or durability.

 

 

Look for:

 

Synthetic Cubic Zirconia:     Hazy transparency, gas bubbles "stingers", read through, and fogs up using the Huff Test.

 

Synthetic Moissanite:           Double refraction is detected through crown facets. Silk like inclusions. High dispersion (the fire) unlike diamond.

 

Synthetic Diamond:              shares the identical, optical, chemical, and physical properties of natural diamonds. Detection of synthetic diamond is very difficult. Testing procedures involve evaluation of magnetic properties, fluorescence patterns and the identification of diagnostic inclusions.

 

Moissanite:                            Silicon Carbide - SiC

Natural occurrence is extremely rare first found as tiny crystals in the analyzes of the Diablo Canyon meteorite in 1893. Synthetic gem quality Moissanite is created exclusively by Charles & Colvard, Inc.

 

Zircon:                                    Zirconium silicate - ZrSiO4

Often mistaken for Synthetic Cubic Zirconia

History of Diamond:

 

 

Discovery: 

 

The first river-bed (alluvial) diamonds were probably discovered in India, in around 800 B.C. The volcanic source of these diamonds was never discovered, but the alluvial deposits were rich enough to supply most of the world's diamonds until the eighteenth century, when dwindling Indian supplies probably spurred the exploration that led to the discovery of diamonds in Brazil, which became the next important diamond source. Beginning in l866, South Africa's massive diamond deposits were discovered, and a worldwide diamond rush was on. The South African diamond output was unrivaled until major deposits were found in Siberian permafrost in l954. And currently Western Canada is the site of the world's newest diamond rush.

 

Throughout much of history, diamonds were mined from the sand and gravel surrounding rivers. But in South Africa in 1870 diamond was found in the earth far from a river source, and the practice of dry-digging for diamonds was born. More sophisticated mining techniques allowed deeper subterranean digging, as well as more efficient river (and, most recently, marine) mining, than ever before.

 

Cutting:

 

The cutting of diamonds into the complex facetted forms we now associate with these gems is actually a relatively recent practice. For centuries, rough diamonds were kept as talismans, and often not worn at all, though natural octahedral (eight-sided stones) were sometimes set in rings. A Hungarian queen's crown set with uncut diamonds, dating from approximately l074, is perhaps the earliest example of diamond jewelry. We know that the royalty of France and England wore diamonds by the 1300's. In sixteenth century England, fashionable lovers etched romantic pledges on windowpanes with the points of their diamond rings, known as "scribbling rings".

 

The earliest record of diamond polishing (with diamond powder) is Indian, and probably dates from the fourteenth century. There are also contemporary references to the practice of diamond polishing in Venice. The earliest reference to diamond cutting is in l550 in Antwerp, the most important diamond center of the period, where a diamond-cutters' guild was soon to be established.

Diamond Routes and Centers:

 

Indian diamonds reached Venice by two Mediterranean routes, the southern route was by way of Aden, Ethiopia, and Egypt, and the northern route was through Arabia, Persia, Armenia, and Turkey. Then, thanks to the Portuguese discovery of the direct sea route to India, Antwerp flourished as a diamond center, as the city was well situated to receive vast supplies of rough from Lisbon as well as from Venice.

 

After Spanish attacks on Antwerp in1585, many diamond cutters relocated to Amsterdam