Diamond Natural History
When it comes to the world of jewelry, and specifically gems such as the diamond, one of the things that make them even more interesting than their mere visual beauty is the fact that there is such a great body of natural history which goes along with each mineral that we know of. Diamonds are among the most fascinating of stones because they are formed from a relatively common element, Carbon. However, despite how common this element might be, it undergoes an incredible process before it will be turned into a diamond.
Diamonds are most often formed more than 93 miles (150 kilometers) beneath the surface of Earth. Scientists believe that carbon, like other elements that make up the planet, came from other stars and intergalactic materials that took part in the Earth’s formation billions of years ago. Down in this mantle level of the earth, the carbon was subjected to impressively high levels of heat and pressure between Earth’s solid crust and its molten core. As a result of all this stress, diamonds crystallized are the densest mineral known by humanity. Other diamonds, such as those found on the continents of South America or Africa, are believed to have been created by meteorites which slammed into Earth and would have had the heat and pressure needed to create the gems.
Since diamonds are so far down, mankind would not have been able to discover them if it were not for certain volcanoes with very deep roots that reach down into the planet’s mantle. The rising lava pulls the raw diamond materials upward towards the crust where it is more accessible to miners. The material that we mine diamonds from is called kimberlite.
While historically, Borneo and India were the only countries where diamonds were mined, discoveries in the 17th Century led to diamonds being found first in South Africa and then across the world. Today 27 nations produce diamonds and they can come from every continent except Europe or Antarctica. When they were first being studied, diamond mines were determined due to blue rocks which would later be called kimberlite after the town of Kimberley, South Africa, near where they were first discovered. When mining for diamonds, there are several minerals that are looked for: olivine, garnet and zircon. All of these could indicate a nearby diamond ‘pipe’, the name given to the tubes of solidified magma that holds kimberlite. For the most part, erosion is what lead to man’s discovery of diamond deposits since they are traditionally quite deep in the planet’s crust.
The first diamonds were discovered by people in India and Borneo, alongside rivers, nearly two millenniums ago, billions of years after natural history says they were formed. It would be more than seventeen centuries later before diamond deposits were uncovered in the rivers of Brazil and for over 140 years, South America would reign supreme as the world’s largest supplier of diamonds. The boom created by diamond discoveries in Africa towards the end of the 1800’s, meant greater understanding of how diamonds originated and lead to many more discoveries around the world until today, miners around the world know precisely what to look for in their pursuit of Earth’s most treasured gemstone.