Mineral
Diamond
Native Element Minerals
Diamond is a mineral form of pure carbon whose atoms are arranged in a crystal structure called diamond cubic. It has the highest hardness and thermal conductivity of any natural material, which is why it is used in cutting and polishing tools as well as in jewelry, and it is colorless in its pure form. A small number of impurities or defects can tint a stone blue (boron), yellow (nitrogen), brown (defects) or green (radiation exposure). Most natural diamonds are between 1 billion and 3.5 billion years old and formed 150 to 250 kilometres down in the Earth's mantle, then were carried to the surface in volcanic eruptions and deposited in rocks known as kimberlites and lamproites. Graphite is the stable form of carbon at room temperature and pressure, and diamond converts to it only at a negligible rate. About 80 percent of mined diamonds are unsuitable as gemstones and are used industrially.
Facts
Formation ClassNative element mineral, a crystalline allotrope of carbon 2 Chemical Formula Hardness (Mohs)Diamond is the reference mineral that defines the value of 10, the hardest end of the Mohs scale. Classification
Strunz Class Crystal System UseIndustrial and Abrasive 1 Connections
Associated With
Primary host rock (main host matrix) for diamond.
Source Kimberlite (Wikipedia)
Diamond-bearing kimberlite pipes bring up peridotite nodules/xenoliths from mantle depth; diamond forms within this peridotite mantle source rock.
Source Peridotite (Wikipedia)
Caused By
Source Diamond Mineral (Wikipedia)
Source Diamond Mineral (Wikipedia)
Classified As
Crystallizes In System
In Discipline
Source Mineral (Wikipedia)
In the Other Atlases
Mineral Species Of
Also in Divinity Atlas: of this mineral species.
Found In
Also in Geography Atlas: where this subject is found.
Source Geology.com: Diamond mineral and gemstoneArticle textQuote, Article text
Argyle diamonds: Octahedral diamond crystals from the Argyle Mine of Western Australia
Also in Geography Atlas: where this subject is found.
Source Geology.com: Diamond mineral and gemstoneArticle textQuote, Article text
Diamonds are mined in Canada
Also in Geography Atlas: where this subject is found.
Source Geology.com: Diamond mineral and gemstoneArticle textQuote, Article text
From the Udachnaya Mine, Yakutia, Siberia, Russia
Sources
1. Diamond Mineral (Wikipedia)
Infobox: system
Cubic
Diamond Mineral (Wikipedia), Industry section
used for adornment, and as industrial abrasives for cutting hard materials
Lead section
Diamond is a mineral form of the element carbon with its atoms arranged in a crystal structure called diamond cubic.
Caused By: Metasomatism, Formation and growth
Diamonds in the mantle form through a metasomatic process
Caused By: Ultra-High-Pressure Metamorphism, Geology
Some blocks of the crust, or terranes, have been buried deep enough as the crust thickened so they experienced ultra-high-pressure metamorphism. These have evenly distributed microdiamonds that show no sign of transport by magma.
View the Source2. Mineral (Wikipedia)
3. minerals.net: Diamond
minerals.netColor field
Colorless, white, yellow, and brown, gray, and black. Colorless Diamonds are usually lightly tinged with yellow, orange or brown. Rarely blue, green, red, orange, pink, or purple.
Luster field
Adamantine. Rough stones have a greasy luster.
View the Source 4. Geology.com: Diamond mineral and gemstone
Geology.comDescriptionQuote, Description
Diamond is a rare, naturally occurring mineral composed entirely of carbon.
View the Source Wikidata: Diamond
Wikidata Q5283
Kimberlite (Wikipedia)
Wikimedia FoundationAssociated With: Kimberlite, Lead sectionQuote, Associated With: Kimberlite, Lead section
It is most commonly known as the main host matrix for diamonds.
View the Source Peridotite (Wikipedia)
Wikimedia FoundationAssociated With: Peridotite, Body, mantle-xenolith discussionQuote, Associated With: Peridotite, Body, mantle-xenolith discussion
The compositions of peridotite nodules found in certain basalts are of special interest along with diamond pipes (kimberlite), because they provide samples of Earth's mantle brought up from depths ranging from about 30 km to 200 km or more.
View the Source Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.
Sign in to dispute this or suggest a correction.