Diamond
![A [[rough diamond]]{{efn|The brownish hue is due to superficial ferrous impurities that constitute evidence of the geological sedimentary context in which it was found. This diamond is potentially colourless.<ref>{{cite web|website=Royal Treasure Museum|title=Gold and Diamonds from Brazil|url=https://www.tesouroreal.pt/en/pages/b9ed8b00-ouro-e-diamantes-do-brasil|access-date=April 18, 2025|url-status=live}}</ref>}}](https://upload.wikimedia.org/wikipedia/commons/b/b7/Rough_Diamond.jpg)
Because the arrangement of atoms in diamond is extremely rigid, few types of impurity can contaminate it (two exceptions are boron and nitrogen). Small numbers of defects or impurities (about one per million of lattice atoms) can color a diamond blue (boron), yellow (nitrogen), brown (defects), green (radiation exposure), purple, pink, orange, or red. Diamond also has a very high refractive index and a relatively high optical dispersion.
Most natural diamonds have ages between 1 billion and 3.5 billion years. Most were formed at depths between in the Earth's mantle, although a few have come from as deep as . Under high pressure and temperature, carbon-containing fluids dissolved various minerals and replaced them with diamonds. Much more recently (hundreds to tens of million years ago), they were carried to the surface in volcanic eruptions and deposited in igneous rocks known as kimberlites and lamproites.
Synthetic diamonds can be grown from high-purity carbon under high pressures and temperatures or from hydrocarbon gases by chemical vapor deposition (CVD). Natural and synthetic diamonds are most commonly distinguished using optical techniques or thermal conductivity measurements. Provided by Wikipedia
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20Published 1995Other Authors: “…Diamond…”