Diamond (gemstone): Difference between revisions
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Diamonds are made of carbon. However, their strength comes from the crystal [[lattice]], that is, the spatial arrangement of carbon [[atoms]], and not from the carbon itself. [[Graphite]], which is the stable form of carbon at surface conditions, is very soft and maleable. In diamonds, each carbon atom (neutral carbon has six [[protons]] and six [[electrons]]; four of the electrons are in the [[valence shell]]), shares all of its valence electrons with a neighboring carbon atom, forming a structure called a [[covalent bond]]. | Diamonds are made of carbon. However, their strength comes from the crystal [[lattice]], that is, the spatial arrangement of carbon [[atoms]], and not from the carbon itself. [[Graphite]], which is the stable form of carbon at surface conditions, is very soft and maleable. In diamonds, each carbon atom (neutral carbon has six [[protons]] and six [[electrons]]; four of the electrons are in the [[valence shell]]), shares all of its valence electrons with a neighboring carbon atom, forming a structure called a [[covalent bond]]. | ||
The exact quantifiable hardness of a diamond is difficult to measure. Although it scores 10 on the [[Mohs scale of hardness]], a diamond's strength can only be measured by itself, as only a diamond can scratch another diamond. | The exact quantifiable hardness of a diamond is difficult to measure. Although it scores 10 on the [[Mohs' scale of hardness]], a diamond's strength can only be measured by itself, as only a diamond can scratch another diamond. | ||
Trace elements may be present and affect the outcome and strength of the composition. The constitution of these trace elements also determines their color, which is proportional to their inherent value. | Trace elements may be present and affect the outcome and strength of the composition. The constitution of these trace elements also determines their color, which is proportional to their inherent value. | ||
Revision as of 13:32, 5 February 2008
This article is about diamonds themselves. For politics surrounding the gemstone trade, see Gemstones (politics).
Diamond, a type of precious gemstone, is the hardest naturally occurring substance found on Earth. They are regarded for their brilliance and their hardness in terms of both appearance and utility. Diamonds are naturally formed from amounts of highly compressed carbon found below into the Earth's mantle (roughly 160 km below the surface), and are brought into the crust by explosive volcanic eruptions. They are typically found in kimberlites (a mixture of different kinds of volcanic rock) within ancient volcanic conduits exposed by erosion.
Synthetic diamonds can be formed in a high-temperature, high-pressure chamber that replicates the geologic conditions which produces them.[1] Synthetic diamonds are very important for industrial applications as abrasives.
Diamonds are made of carbon. However, their strength comes from the crystal lattice, that is, the spatial arrangement of carbon atoms, and not from the carbon itself. Graphite, which is the stable form of carbon at surface conditions, is very soft and maleable. In diamonds, each carbon atom (neutral carbon has six protons and six electrons; four of the electrons are in the valence shell), shares all of its valence electrons with a neighboring carbon atom, forming a structure called a covalent bond.
The exact quantifiable hardness of a diamond is difficult to measure. Although it scores 10 on the Mohs' scale of hardness, a diamond's strength can only be measured by itself, as only a diamond can scratch another diamond.
Trace elements may be present and affect the outcome and strength of the composition. The constitution of these trace elements also determines their color, which is proportional to their inherent value.
Diamonds can be found in these colors: "clear" (or white), yellow, brown, green, pink, blue and very rarely, red. "Raw" diamonds only slightly resemble a finished diamond: there may be a hint of color or a small section that is crystallized.
Diamonds have been found in South Africa, India, Indonesia, China, Russia, Australia, Brazil, California, Colorado, and Canada.
References
- ↑ Davis, Joshua (2003-09-01). The New Diamond Age - How to Make a Diamond: The Gemesis Way. Wired Magazine. Retrieved on 2007-12-28.