The slightly misshapen octahedral shape of this rough diamond crystal in matrix is typical of the mineral. Its lustrous faces also indicate that this crystal is from a primary deposit.
|Color||Typically yellow, brown or gray to colorless. Less often blue, green, black, translucent white, pink, violet, orange, purple and red.|
|Crystal system||Isometric-Hexoctahedral (Cubic)|
|Twinning||Spinel law common (yielding "macle")|
|Cleavage||111 (perfect in four directions)|
|Mohs scale hardness||10 (defining mineral)|
|Diaphaneity||Transparent to subtransparent to translucent|
|Refractive index||2.418 (at 500 nm)|
|Melting point||Pressure dependent|
Diamonds have the highest hardness of any bulk (all one type) material. Because of this, many important industries use diamonds as tools for cutting and polishing things. Many of them are clear, but some of them have colors, like yellow, red, blue, green and pink. Diamonds of a different color are called "fancies".
Big diamonds are very rare, and are worth a lot of money. Only 20% of diamonds are fit for jewellery. The other 80% are not pretty enough. They are industrial diamonds, used to make things like drill bits and diamond saws. This is because even a diamond that is not beautiful is useful because It is very hard.
Because many diamonds are beautiful, people make jewellery using them. Diamonds are very effective electrical insulators, but also very good conductors of heat. On Mohs scale of mineral hardness, diamonds are scored as 10 (the highest score possible).
Formation of diamondsEdit
There are natural and synthetic diamonds. The Earth makes natural diamonds, and people make synthetic diamonds. Diamonds are the hardest natural substance known to man. Diamonds are made of pure carbon, the same chemical element as graphite, fullerene, and coal. But diamonds are very hard and in crystalline form. It is commonly believed that diamonds are formed from coal, but this is not true.
Diamonds are made deep in the Earth where there is an intense amount of pressure and heat. The formation of natural diamonds needs specific conditions. These are exposure of carbon-bearing materials to high pressure, between 45 and 60 kilobars (4.5 and 6 GPa), but at a comparatively low temperature, between about 900 and 1,300 °C (1,650 and 2,370 °F). These conditions are found in two places on Earth: in the lithospheric mantle below relatively stable continental plates, and at the site of a meteorite strike.
People find diamonds where volcanoes were a long time ago. They sometimes find tiny ones at the site of a meteorite strike. Sometimes people find diamonds on the top of the ground. But in places like South Africa, they must dig deep down into a diamond mine to get diamonds. Diamonds were first found in India.
Small synthetic diamonds are made for abrasives. Large synthetic ones are even more expensive to make than to find and dig up, so people don't make large synthetic diamonds.
Trading in diamondsEdit
For many decades the trading of diamonds was controlled by the De Beers group of companies, who controlled most of Africa's rich diamond mines. However, in the late 1980s and early 1990s, new diamond mines opened in Canada and Australia that De Beers wasn't able to control. When the USSR collapsed in 1991, many cheap Russian diamonds entered the market, overwhelming De Beers and their efforts to control it. De Beers still runs most of Africa's diamond mines, but their mines now only produce about one third of the world's diamonds.
- "Diamond". Mindat. Retrieved July 7, 2009.
- "Diamond". WebMineral. Retrieved July 7, 2009.
- Carlson R.W. 2005. The mantle and core. Elsevier. p. 248. ISBN 0-08-044848-8. https://books.google.com/?id=1clZ4ABsfoAC&pg=PA248.
- Zimnisky, Paul (June 06, 2013). "A Diamond Market No Longer Controlled By De Beers". Check date values in:
|The Simple English Wiktionary has a definition for: diamond.|