allotrope of carbon often used as a gemstone and an abrasive

A diamond (from the ancient Greek αδάμας – adámas "unbreakable") is a re-arrangement of carbon atoms (those are called allotropes).

A clear octahedral stone protrudes from a black rock.
The slightly uneven eight-sided 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.
(repeating unit)
Strunz classification01.CB.10a
Molecular mass12.01 g/mol
ColorTypically yellow, brown or gray to colorless. Less often blue, green, black, translucent white, pink, violet, orange, purple and red.
Crystal habitOctahedral
Crystal systemIsometric-Hexoctahedral (Cubic)
TwinningSpinel law common (yielding "macle")
Cleavage111 (perfect in four directions)
FractureConchoidal (shell-like)
Mohs scale hardness10 (defining mineral)
DiaphaneityTransparent to subtransparent to translucent
Specific gravity3.52±0.01
Density3.5–3.53 g/cm3
Polish lusterAdamantine
Optical propertiesIsotropic
Refractive index2.418 (at 500 nm)
Melting pointPressure 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 of lower quality. Those lower quality diamonds are called industrial diamonds, and are used to make things like drill bits and diamond saws. Even if a diamond is not of gem quality, it still has a value because It is very hard.

Cut and faceted diamonds can be attractive hence their use in jewellery. 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 diamonds change

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.[3]

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 diamonds change

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.[4]

References change

  1. "Diamond". Mindat. Retrieved July 7, 2009.
  2. "Diamond". WebMineral. Retrieved July 7, 2009.
  3. Carlson R.W. 2005 (22 November 2005). The mantle and core. Elsevier. p. 248. ISBN 0-08-044848-8.{{cite book}}: CS1 maint: numeric names: authors list (link)
  4. Zimnisky, Paul (June 6, 2013). "A Diamond Market No Longer Controlled By De Beers". Archived from the original on 2020-10-07.

Other websites change