Diamonds
Diamond is entirely made of Carbon atoms (Chemical Composition - 'C') crystallised in a cubic (isometric) arrangement. Most natural diamonds are formed at high-pressure high-temperature environments existing at depths of 140 to 190 kilometers (87 to 120 mi) in the Earth mantle. Diamond deposits are termed Kimberlite Pipes or Blue Ground. These are also called Primary Mines. In contrast, diamonds are also found at river beds. These are Alluvial Deposits.
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