Diamonds from outer space.What do you get when a massive comet collides with Earth? Billions of diamonds! Scientists really "dig" this dazzling phenomenon. Science isn't always glitter and glitz glitz Informal n. Ostentatious showiness; flashiness: "a garish barrage of show-biz glitz" Peter G. Davis. tr.v. . But in a while, scientists discover something truly spectacular--like diamonds! Recently, geologists (earth scientists) discovered billions of diamonds where no one before. had thought to search. They found the diamonds in craters, basins pounded into Earth's surface Noun 1. Earth's surface - the outermost level of the land or sea; "earthquakes originate far below the surface"; "three quarters of the Earth's surface is covered by water" surface when speeding rocks from outer space smash into our planet. Traditionally, mining companies dig up diamonds from deep below Earth's surface. But the newly discovered diamonds are a sparkling surprise. They lie encased en·case tr.v. en·cased, en·cas·ing, en·cas·es To enclose in or as if in a case. en·case ment n. in rock right on the surface, says Virgil. Sharpton, a geophysicist at the Lunar and Planetary Institute The Lunar and Planetary Institute (LPI) is a NASA-funded research institute, dedicated to studies of the solar system, its evolution and formation. The Institute is part of the Universities Space Research Association, located in Houston, Texas. in Houston. Scientists have dubbed their discovery "impact diamonds" because they form during impacts of comets, asteroids This is a list of numbered minor planets, nearly all of them asteroids, in sequential order.As of late September 2007 there are 164,612 numbered minor planets, and many more not yet numbered. Most asteroids are ordinary and not particularly noteworthy. , or meteors. Russian scientists discovered. the first impact diamonds about 20 years ago, says Richard A.F. Grieve, al research scientist at the Geological Survey The term geological survey can be used to describe both the conduct of a survey for geological purposes and an institution holding geological information. A geological survey of Canada. A group of prospectors had been analyzing rocks near a crater in Siberia. While viewing the rocks under a microscope, they realized the rocks contained diamonds. The Russians kept their treasure secret for two decades. But now the word is out, thanks to greater communication with Russian scientists since the end of the Cold War. And over the past decade, geologists have uncovered impact diamonds in more than half a dozen giant craters around the globe. Despite the huge size of these treasure troves TREASURE TROVE. Found treasure. 2. This name is given to such money or coin, gold, silver, plate, or bullion, which having been hidden or concealed in the earth or other private place, so long that its owner is unknown, has been discovered by accident. , scientists don't expect to strike it rich any time soon. "Most of the impact diamonds are smaller than the head of a pin," Sharpton says. Some are microscopic--tinier than viruses! As one scientist jokes, "They'd make good engagement rings for an ant, but Liz Taylor wouldn't be very impressed." Still, scientists are excited because the impact diamonds tell a tale about Earth's history. COSMIC COLLISIONS Believe it or not, our planet is constantly being bombarded with rocky objects from outer space, Sharpton explains. "Most of the objects that come close to Earth are so small they either burn up in our atmosphere or rain down as small meteorites Meteorites See also astronomy. aerolithology the science of aerolites, whether meteoric stones or meteorites. Also called aerolitics. astrolithology the study of meteorites. Also called meteoritics. . "It's very rare," Sharpton continues, "that you find an object large enough to make it through Earth's atmosphere “Air” redirects here. For other uses, see Air (disambiguation). Earth's atmosphere is a layer of gases surrounding the planet Earth and retained by the Earth's gravity. It contains roughly (by molar content/volume) 78% nitrogen, 20.95% oxygen, 0.93% argon, 0. and strike the Earth with such velocity that it produces a crater." But the 150 impact craters scientists have mapped around the globe over the past 50 years are evidence that such collisions do occur. (The most recent major impact was probably some 50,000 years ago.) Though scientists discover only three to five craters each year, hundreds more may dot the planet. These include many craters that wind and water have eroded, or worn away, over time. That's where impact diamonds come in. Finding them is like finding "'fingerprints' of an impact event," Sharpton says. It's as if the diamonds hold up a sign that says, "A cosmic collision happened here." UNDER PRESSURE The diamonds are also signposts of the enormous heat and pressure that result when a large space rock crashes, says Grieve. Intense heat and pressure, after all, are essential to diamond formation. So is the element carbon, diamond's main ingredient. These materials and conditions certainly exist where diamonds usually form, deep within our planet (see diagram, opposite page). Some 160 kilometers (100 miles) beneath the crust, in the mantle. Earth's thickest layer, temperatures soar as high as 1,000[degrees]C (1,832[degrees]F). That's hot enough to melt rock and form magma, the semi-melted ooze OOZE - Object oriented extension of Z. "Object Orientation in Z", S. Stepney et al eds, Springer 1992. that churns beneath Earth's surface. In addition, the enormous weight of rocks pressing down creates pressure in the mantle that's tens of thousands of times Earth's atmospheric pressure atmospheric pressure or barometric pressure Force per unit area exerted by the air above the surface of the Earth. Standard sea-level pressure, by definition, equals 1 atmosphere (atm), or 29.92 in. (760 mm) of mercury, 14.70 lbs per square in., or 101. at sea level. The intense heat and pressure "cook" and squeeze atoms of carbon in certain rocks and minerals (like limestone and graphite) within the magma. The heat and pressure actually rearrange re·ar·range tr.v. re·ar·ranged, re·ar·rang·ing, re·ar·rang·es To change the arrangement of. re the carbon atoms so that they form repeating patterns with flat sides, or faces--crystals. Voila, a diamond is born! Explosions of gas within Earth's mantle sometimes force these diamonds and surrounding rocks closer to the surface. FAST TRACK Diamonds can take millions of years to form underground, Sharpton says. But a cosmic collision can create diamonds in just a fraction of a second. The pressure created by a comet colliding is more than a million times the atmospheric pressure at sea level. The impact forces a huge cloud of dust, rock, and vapor into the air. "You can compare this cloud to a mushroom cloud that forms after a nuclear explosion," Grieve says. (Scientists suspect that the huge amount of debris from one such collision 65 million years ago may have cast a haze around the globe and wiped out the dinosaurs.) Based on computer models, scientists think that temperatures in the cloud Refers to the operation taking place within a network. See cloud. may reach 4,000[degrees]C (7,232[degrees]F. As the cloud cools, carbon blasted from either graphite or limestone on the ground can crystallize crys·tal·lize also crys·tal·ize v. crys·tal·lized also crys·tal·ized, crys·tal·liz·ing also crys·tal·iz·ing, crys·tal·liz·es also crys·tal·iz·es v.tr. 1. to form diamonds. This split-second crystallization Crystallization The formation of a solid from a solution, melt, vapor, or a different solid phase. Crystallization from solution is an important industrial operation because of the large number of materials marketed as crystalline particles. is one reason the impact diamonds are so small, Grieve says. The crystals don't have time to form repeating layers and "grow." Even the rare few impact diamonds that are as large as peanuts are "messy looking things," he adds. They're full of cracks and impurities like gas bubbles and traces of carbon that failed to crystallize. Not exactly jewel quality. Still, the impact diamonds could be valuable. They're just as hard as other diamonds. So companies may one day use them for industrial purposes, like cutting steel to make cars, airplanes, and other machines. Industries already use more than half of all 18,000 kilograms (40,000 pounds) of diamonds mined around the world each year. Only a small percent are made into jewelry. So far, geologists have uncovered the largest batch of impact diamonds in a crater in Siberia. Other groups are searching for craters--and diamonds--in Europe and Canada. The U.S. hunt may begin soon. If your house lies on an unmapped crater, you could be standing on a field of gems! RELATED ARTICLE: Fab Facts * Diamonds are the hardest substance on Earth. The word "diamond" comes from the Greek word adamas, which means "invincible." * In 1867, a young boy in South Africa South Africa, Afrikaans Suid-Afrika, officially Republic of South Africa, republic (2005 est. pop. 44,344,000), 471,442 sq mi (1,221,037 sq km), S Africa. found a "pretty pebble" near a river. It turned out to be a $2,500 diamond. * The largest diamond ever discovered weighed about 0.6 kilograms (1.3 pounds). Cutters divided the diamond into nine large gems and 96 smaller stones. * The world's largest known impact crater lies completely under water off the Yucatan Peninsula of Mexico. The crater measures more than 300 kilometers (200 miles) in diameter. * If temperatures rise above 1,000[degrees]C (1,832[degrees]F), diamonds will combine with oxygen and burn. The product will be ordinary carbon dioxide carbon dioxide, chemical compound, CO2, a colorless, odorless, tasteless gas that is about one and one-half times as dense as air under ordinary conditions of temperature and pressure. gas! RELATED ARTICLE: Where Diamonds Form Inside Earth The high temperature and pressure 160 kilometers (100 miles) below Earth's surface are perfect for diamond formation. There, in the upper mantle, the heat and pressure "cook" and squeeze carbon atoms in semimelted rocks. Sometimes these conditions rearrange the carbon atoms to form the repeating layers of flat-sided crystals--diamonds. Explosions of gas within the mantle can carry these diamonds and surrounding rocks to the surface. Deeper inside Earth, in the lower mantle Noun 1. lower mantle - the deeper part of the mantle layer - a relatively thin sheetlike expanse or region lying over or under another mantle - the layer of the earth between the crust and the core or the core, temperatures are too high for diamonds to form. There the carbon would burn or melt. [ILLUSTRATION OMITTED] |
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