On your next trip to the local shopping mall, stop by one
of the jewelry stores. Notice the diamond jewelry that takes
up the majority of the showcase, and the number of people
hovering over the counters trying to pick out a diamond for
their loved one. There will surely be a salesperson explaining
the "4 Cs" -- cut, clarity, carat
and color -- to a young shopper, and explaining why one
diamond is better than the one right next to it. Why all the
fuss over diamonds?
Photo courtesy Smithsonian Institution/Chip
Clark The Hooker Diamond
necklace, earrings and ring on display at the National
Museum of Natural
History
Diamonds are just carbon in its most concentrated
form. That's it -- carbon, the element that makes up 18
percent of the weight of your body. In many countries,
including the United States and Japan, there is no other
gemstone as cherished as the diamond, but in truth, diamonds
are no more rare than many other precious gems. They continue
to demand higher market prices because the majority of the
diamond market is controlled by a single entity.
In this edition ofHowStuffWorks,
we will track a diamond from the time it is formed to when it
reaches the Earth's surface. We will also examine the
artificial rarity created by the diamond cartel, De
Beers, and briefly discuss the properties of these gems.
The Origin of Diamonds Carbon is one of the
most common elements in the world, and is one of the four
essentials for the existence of life. Humans are more than
18-percent carbon. The air we breathe contains traces of carbon. When occurring in
nature, carbon exists in three basic forms:
Diamond - an extremely hard, clear crystal
Graphite - A soft, black mineral made of pure
carbon. The molecular structure is not as compact as
diamond's, which makes it weaker than diamond.
Fullerite - A mineral made of perfectly spherical
molecules consisting of exactly 60 carbon atoms. This
allotrope was discovered in 1990.
Archean
Cratons
Temperatures can
reach 1,652 F (900 C) in Archean cratons. These
are common places for diamonds to form. Archean cratons
are stable, horizontal geological formations created
billions of years ago that have been unaffected by major
tectonic events, according to Rex Diamond Mining Corp.
These cratons are found in the
center of most of the seven continents (most tectonic
activity takes place around the
edges).
Diamonds
form about 100 miles (161 km) below the Earth's surface, in
the molten rock of the Earth's mantle, which provides the right amounts of pressure and
heat to transform carbon into a diamond. In order for a
diamond to be created, carbon must be placed under at least
435,113 pounds per square inch (psi or 30 kilobars) of
pressure at a temperature of at least 752 degrees Fahrenheit
(400 Celsius). If conditions drop below either of these two
points, graphite will be created. At depths of 93 miles (150
km) or more, pressure builds to about 725,189 psi (50
kilobars) and heat can exceed 2,192 F (1,200 C).
Most diamonds that we see today were
formed millions (if not billions) of years ago. Powerful magma
eruptions brought the diamonds to the surface, creating
kimberlite pipes. Kimberlite is named after Kimberly,
South Africa, where these pipes were first found. Most of
these eruptions occurred between 1,100 million and 20 million
years ago.
Space
Diamonds
Diamonds are
not exclusive to Earth. Scientists believe that diamonds
may one day be found on the moon. Samples of rock
brought back from the moon indicate that carbon is 10
times more abundant in the Earth's crust than the
moon's, according to the Artemis
Project, a group whose goal is to establish a
permanent moon community. But this group believes that
there may be diamonds under the moon's surface that
Apollo astronauts were unable to detect.
There is also some scientific evidence that diamonds
may be found in larger abundance on Neptune and
Uranus. Neptune and Uranus contain a lot of the
hydrocarbon gas methane. Researchers at the
University of California, Berkeley, have shown that focusing a laser beam on
pressurized liquid methane can produce diamond dust.
Neptune and Uranus contain about 10-percent to
15-percent methane under an outer atmosphere of hydrogen
and helium. Scientists think that this methane could
possibly turn to diamond at fairly shallow depths. Click
here to learn more about the Berkeley
experiment.
Kimberlite pipes are created as magma
flows through deep fractures in the Earth. The magma inside
the kimberlite pipes acts like an elevator, pushing the
diamonds and other rocks and minerals through the mantle and
crust in just a few hours. These eruptions were short, but
many times more powerful than volcanic eruptions that happen
today. The magma in these eruptions originated at depths three
times deeper than the magma source for volcanoes like Mount
St. Helens, according to the American Museum of Natural
History.
The magma eventually cooled inside these kimberlite pipes,
leaving behind conical veins of kimberlite rock that contain
diamonds. Kimberlite is a bluish rock that diamond miners look
for when seeking out new diamond deposits. The surface area of
diamond-bearing kimberlite pipes ranges from 2 to 146 hectares
(5 to 361 acres).
Diamonds may also be found in river beds, which are called
alluvial diamond sites. These are diamonds that
originate in kimberlite pipes, but get moved by geological
activity. Glaciers and water can also move diamonds thousands
of miles from their original location. Today, most diamonds
are found in Australia, Borneo, Brazil, Russia and several
African countries, including South Africa and Zaire.
Diamonds are found as rough stones and must be processed to
create a sparkling gem that is ready for purchase. In the next
section, you will learn how a diamond is cut and polished.
Diamond Properties As mentioned before,
diamonds are the crystallized form of carbon created under
extreme heat and pressure. It's this same process that makes
diamonds the hardest mineral we know of. A diamond ranks a 10
on the Mohs Hardness Scale (see below). It can be
anywhere from 10 to hundreds of times harder than a mineral
ranked nine on the Mohs scale, such as corundum. Corundum is a
class of minerals that includes rubies and sapphires.
It is the molecular structure of diamonds that makes
them so hard. Diamonds are made of carbon atoms linked
together in a lattice structure. Each carbon atom shares
electrons with four other carbon atoms, forming a
tetrahedral unit. This tetrahedral bonding of five
carbons forms an incredibly strong molecule. Graphite, another
form of carbon, isn't as strong as diamond because the carbon
atoms in graphite link together in rings, where each atom is
only linked to one other atom.
Diamonds are cut along planes of weaknesses
to create the shape and facets of the diamonds we see in
the jewelry
store.
There are special techniques that are used to cut and shape
a diamond before it gets to the jewelry store. Diamond cutting
creates the facets that you see in the diagram above. Diamond
cutters use these four basic techniques:
Cleaving - In order to remove any impurities or
irregularities in the diamond, a rough diamond is placed in
quick-drying cement. A sharp groove is then carved into the
diamond, using another diamond or a laser, along planes of
weakness. Then, a steel blade is placed in the groove and a
sharp blow to the blade splits the stone. It is then removed
from the cement.
Sawing - Sometimes, diamonds have to be cut
against a cleavage plane, which cannot be done with
cleaving. Using a phosphor-bronze blade rotating at about
15,000 rpm, the saw slowly cuts through the diamond. Lasers
are also being used to saw diamonds.
Bruting - The diamond is placed in a lathe, and
another diamond in the lathe is rubbed against it to create
the rough finish of the girdle, the outside rim of
the diamond at the point of largest diameter.
Polishing - To give the diamond its finished
look, it is placed onto the arm above a rotating polishing
wheel. The wheel is coated with diamond powder that smoothes
the diamond as it is pressed against the wheel.
Diamonds are judged on several factors that determine their
beauty. Most diamonds never reach the consumer market because
they are too flawed. Often, these diamonds are used for
industrial purposes -- as an abrasive, for drill bits or for
cutting diamonds and other gems. If you've ever purchased a
diamond, you've heard of the "4 Cs:"
Cut - This refers to how the diamond has been cut
and its geometric proportions. When a diamond is cut, facets
are created and the diamond's finished shape is determined.
Clarity - This is the measurement of a diamond's
flaws, or inclusions that are seen in the diamond. Clarity
levels begin with Flawless and move down to Very Very Slight
(VVS), Very Slight (VS) and Slightly Included (SI).
Carat - This is the weight of a diamond. One
carat is equal to about 200 milligrams.
Color - In referring to transparent diamonds, the
color scale runs from D to Z, beginning with Icy White --
the color of the most expensive diamonds -- and ending with
a light yellow.
Other unique qualities of the diamond include its
transparency, luster and dispersion of
light. A diamond that is created from 100-percent carbon
will be completely transparent. Diamonds often contain other
elements that can affect the color. Although we often think of
diamonds as being clear, there are also blue, red, black, pale
green, pink and violet diamonds. These colored diamonds are
the truly rare ones.
The Mohs
Scale
The Mohs Scale is
used to determine the hardness of solids, especially
minerals. It is named after the German mineralogist
Friedrich Mohs. The scale reads as follows, from
softest to hardest:
Talc - easily scratched by the fingernail
Gypsum - just scratched by the fingernail
Calcite - scratches and is scratched by a
copper coin
Fluorite - not scratched by a copper coin
and does not scratch glass
Apatite - just scratches glass and is
easily scratched by a knife
Orthoclase - easily scratches glass and is
just scratched by a file
Quartz (amethyst, citrine, tiger's-eye,
aventurine) - not scratched by a file
Topaz - scratched only by corundum and
diamond
Corundum (sapphires and rubies) - scratched
only by diamond
Diamond - scratched only by another diamond
Source: Kingzett's Chemical Encyc.
A Perception of Rarity Diamonds are made in
the molten magma deep inside the Earth. Only nature can create
diamonds, but it is people who have created the artificial
rarity that has spurred demand for these gems. Carbon is one
of the most common elements in the world, and diamonds are a
form of carbon. Naturally occurring diamonds are no more rare
than many other precious gems. The truly rare transparent
diamonds are those rated as flawless, meaning that they don't
have the slightest imperfection.
Photo courtesy Smithsonian
Institution Some diamonds,
like the Hope Diamond (pictured here), are extremely
rare. However, most diamonds are much more abundant than
we are led to
believe.
Diamonds were not always so popular
with the American public, and they were not always so pricey.
A diamond placed in a mounting on a ring has a markup of about
100 percent to 200 percent. The only reason why we pay so much
more for diamonds today than for other precious gems is
because the diamond market is controlled almost entirely by a
single diamond cartel, called De Beers Consolidated Mines,
Ltd., which is based in South
Africa.
De Beers stockpiles diamonds mined from
countries around the world and releases a limited number of
diamonds for sale each year. De Beers produces half of the
world's diamond's supply and controls about two-thirds of the
entire world market, according to a Washington Post report. At times, just to keep prices up, De Beers
has bought tremendous numbers of diamonds from countries
attempting to inject large quantities into the market. If De
Beers were a U.S.-based company, it would be in violation of
antitrust laws for fixing the prices of diamonds.
The secret to De Beers' success is a
marketing campaign that convinces women that they should
receive a diamond ring from their fiancee and convinces young
men to pay "two-months salary" for that ring to show how much
their love is worth. Prior to the 1930s, diamond rings were
rarely given as engagement rings. Opals, rubies, sapphires and
turquoise were deemed much more exotic gems to give as tokens
of one's love, according to the book "Twenty Ads that Shook
the World," by James B. Twitchell.
Twitchell goes on to describe how De Beers changed the world
diamond market.
This idea of connecting diamonds to romance was captured in
a brilliant ad campaign begun in the 1940s, causing demand for
diamonds to increase. Surely you've heard the De Beers
advertisement telling you that "A Diamond is Forever."
This ad campaign, which was created by the N.W. Ayer advertising agency in 1947, changed the diamond
market. In 2000, Advertising Age magazine named the ad campaign the slogan of the 20th
century. De Beers infiltrated Japan with the same ad campaign
in the 1960s, and the Japanese public bought into the idea as
much as the Americans did.
Later ads by De Beers told consumers to hold onto their
family's diamond jewelry and to cherish them as heirlooms --
and it worked. This eliminated the aftermarket for diamonds,
which further enabled De Beers to control the market. Without
people selling their diamonds back to jewelers or to other
people, the demand for new diamonds increased.
There are fewer than 200 people or companies authorized to
buy rough diamonds from De Beers. These people are called
sightholders, and they purchase the diamonds through
the Central Selling Organization (CSO), a subsidiary of De
Beers that markets about 70 percent to 80 percent of the
world's diamonds. De Beers sells a parcel of rough diamonds to
a sightholder, who in turn sends the diamonds to cutting
facilities and then to distributors.
There are rough diamonds sold outside the CSO. These
diamonds come from small producers in Australia, Russia and
some African countries. The cost of these diamonds is still
largely influenced by the prices set by the CSO.
Diamonds are the most coveted of all precious gems, as is
witnessed by the extremely high demand for them. While this
has not always been the case, diamonds are nonetheless
exquisite gems that go through a long, tedious refining
process from the time they are pulled from the ground to when
you see them in the jewelry store. And, while some of the
mystique of diamonds may be gone -- they're just carbon, after
all -- the diamond will likely continue to be a highly coveted
jewel, because, well, "A Diamond is Forever."
Famous Diamonds
The Cullinan - This is the largest diamond ever
found. This 3,106-carat diamond was found in 1905 in
Transvaal, South Africa. In 1907, the diamond was presented
to King Edward VII of England. Later, the diamond was cut
into nine major stones, including the 530.20-carat Star
of Africa diamond that is
set in the Royal Scepter displayed in the Tower of London.
The Hope Diamond - Possibly the most famous
diamond in America, this 45.52-carat diamond is on display
at the National Museum of Natural History in Washington D.C.
Photo courtesy Smithsonian
Institution
Its history dates back to the 1600s, when it was
originally a 112.1875-carat diamond. In 1668, it was
purchased by King Louis XIV,
of France. It is believed to have been originally found in
the Kollur mine in Golconda, India. The diamond was recut in 1673, creating a smaller 67.125-carat stone.
The Excelsior - Perhaps the second-largest
diamond ever found, the Excelsior was found in 1893 in South
Africa. The original stone weighed about 995 carats.
In 1904, I.J. Asscher and Company of Amsterdam cut the
Excelsior into 21 polished stones weighing between 1 and 70
carats.
The Great Mogul - Believed to be the
third-largest uncut diamond ever found, it was discovered
around 1650. Its original size is said to have been
787.50 carats, but it was cut to just 280 carats. The
diamond is named for Shah Jehan, who built the Taj
Mahal. After the diamond was cut, he fired the cutter for
doing such a poor job. Mysteriously, the whereabouts of the
Great Mogul diamond are unknown today.
For more information on diamonds and
related topics, check out the links on the next page.