Diamonds are commonly found in Brazil, Africa, Canada, Russia, and Australia. However, the earliest source of diamonds was in India as early as 800BC, but after the Spanish Conquest, production shifted to Brazil.
They are formed at temperatures between 900 and 1300 degrees Celsius, at a depth of between 90 and 120 miles below the earth’s surface, and at pressures over 45kbar. This is how the oldest diamonds have formed; but diamonds have also been derived from mantle eclogite rock. They grew within this rock, and it is likely that the carbon came from early micro-organisms that lived in the mud of the sea beds.
Just like any other mineral, diamonds retain impurities from the surrounding rock during their growth. This can be anything from single atoms to complete mineral crystals. If they can be seen under an ordinary gemmological microscope, they are known as inclusions. Inclusions are graded so the buyer can get a clear picture regarding diamond quality when they purchase.
There are many qualities that make the diamond superior, however, its hardness sets it apart, as diamonds are the hardest natural substance known. Traditionally, the diamond is the emblem of fearlessness, yet it has also come to be symbolic of love. You can discover all of the information you need to know about this precious gemstone by browsing the Rêve website further.
It is impossible to find a perfect diamond; they all have small impurities, which are known as inclusions. The clarity grading system is used to determine just how many inclusions the diamond has. If the impurities are visible to the naked eye, the diamond will have a very low clarity rating.
There are numerous diamond certificates that are issued to give the buyer accurate details regarding the identity of the diamond, its value, and its technical characteristics. It is important to know about the various certificates and grading bodies so you can understand their standards, and thus what they are judging a diamond on.