Crystals gems5/7/2023 ![]() The Golkonda region in south-central India was the original source of diamonds for hundreds of years, until discoveries were made in Brazil during the 18th century and at Kimberley, South Africa, in 1866. (Common gem materials not addressed in this article include amber, amethyst, chalcedony, garnet, lazurite, malachite, opals, peridot, rhodonite, spinel, tourmaline, turquoise and zircon.) ![]() The desire to unravel the history of such unusual circumstances is drawing increasing numbers of Earth scientists to the study of gems and their origins.Īlthough there are dozens of different types of gems, among the best known and most important are diamond, ruby and sapphire, emerald and other gem forms of the mineral beryl, chrysoberyl, tanzanite, tsavorite, topaz and jade. Exceptional geological conditions are required to produce gem deposits. This scarcity also makes gemstones highly valuable to geologists. For instance, one emerald mine established in 1981 in Santa Terezinha, Brazil, produced a peak of 25 tons of rough stones valued at $9 million in 1988 the same tonnage of stones mined in 2000 sold for only $898,000. Thus high-quality gems can be mined out much faster than they are produced, essentially making them a finite resource. Radioactive-decay dating of microscopic inclusions in diamonds has found these gems to be 970 million to 3.2 billion years old. Like oil, gems can take an immense stretch of geologic time to form. ![]() A typical diamond deposit yields 5 grams of gems per million grams of mined material, with only 20 percent of the gems being of jewelry quality. Part of the reason that gemstones reach such high values is their rarity. Although synthetic forms of many gems now exist, they have yet to have a serious impact on the international gemstone market. However, world production of uncut diamonds was worth $12.7 billion in 2008, and in 2001 the trade journalĬalculated that the world colored-gem trade was worth about $6 billion per year. ![]()
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