Diamond (gemstone): Difference between revisions
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''This article is about diamonds themselves. For politics surrounding the gemstone trade, see [[Gemstones (politics)]].'' | ''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 the Earth's [[mantle | '''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 the Earth's [[mantle (geology)|mantle]] (roughly 100 miles below the surface), but synthetic diamonds can be formed in a high-temperature, high-pressure chamber that replicates the geologic conditions which produces them.<ref>{{cite web|url=http://www.wired.com/wired/archive/11.09/diamond.html?pg=6&topic=&topic_set=title=|title=The New Diamond Age - How to Make a Diamond: The Gemesis Way|publisher=Wired Magazine|date=2003-09-01|accessdate=2007-12-28|author=Davis, Joshua}}</ref> | ||
Diamonds are mostly made from carbon. However, their strength comes from the crystal structure of carbon [[atoms]] and not from the carbon itself ([[graphite]], for example, 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 mostly made from carbon. However, their strength comes from the crystal structure of carbon [[atoms]] and not from the carbon itself ([[graphite]], for example, 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]]. | ||
Revision as of 05:55, 2 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 the Earth's mantle (roughly 100 miles below the surface), but synthetic diamonds can be formed in a high-temperature, high-pressure chamber that replicates the geologic conditions which produces them.[1]
Diamonds are mostly made from carbon. However, their strength comes from the crystal structure of carbon atoms and not from the carbon itself (graphite, for example, 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.