The Start Of Diamonds - 0 views

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  #1 Atkins Kirkpatrick on 15 Jan 14

   

  Diamonds are formed under very specific problems that need materials displaying carbon to be subjected to high pressure although low temperature (relative to most areas deep in the earth.) the temperature no less than 1652 degrees Fahrenheit and The pressure must be somewhere at the least 45 kilobars. You can find only two circumstances that provide these settings in the Earth. They are in the site of the attack by a meteorite or inside the earths lithospheric mantle and where it's below continental plates that are fairly stable.
  
  Diamonds are only produced deep inside the earth, a minimum of 9-0 miles down, to a maximum of 120 miles deep. Of-course, this depends on the geographic area as the rate of temperature change relative to depth is different in different locations. Under oceanic plates, like, the temperature will increase more quickly when you go deeper in the earth. The only place where you'll find the ideal mix of temperature and pressure are the most secure and oldest, thickest parts of the earths continental dishes where lithosphere areas called cratons are found. The longer the diamond crystals reside in the cratons the bigger the diamonds that result.
  
  The carbon that individuals find in diamonds originates from a variety of both organic and inorganic matter. Scientists have determined this by studying rates of carbon isotopes, a method somewhat similar to carbon dating. Some diamonds, named harzburgitic, have been formed from carbon that is inorganic and within the deepest areas of the earths layer. Eclogitic diamonds, in contrast, include organic carbon that comes from organic detritus being pressed by subduction from the surface of the planet earth. Diamonds that rise to the outer lining of the planet earth have reached least one billion years old and could be over three billion years.
  
  Sometimes diamonds type in other events that also have high-pressure and low temperature adjustments. Nanodiamonds and microdiamonds, the very smallest of the stone family, have already been identified inside impact craters, the consequence of meteors striking our planet. Visiting online consumer discounts probably provides tips you should give to your cousin. The shock of the meteor strikes actually produces the perfect temperature and pressure conditions that induce these diamonds.
  
  Source: http://en.wikipedia.org/wiki/Diamond.

   

  <div class="cArrow"> </div><div class="cContentInner">Diamonds are formed under very specific problems that need materials displaying carbon to be subjected to high pressure although low temperature (relative to most areas deep in the earth.) the temperature no less than 1652 degrees Fahrenheit and The pressure must be somewhere at the least 45 kilobars. You can find only two circumstances that provide these settings in the Earth. They are in the site of the attack by a meteorite or inside the earths lithospheric mantle and where it's below continental plates that are fairly stable. <br /> <br /> Diamonds are only produced deep inside the earth, a minimum of 9-0 miles down, to a maximum of 120 miles deep. Of-course, this depends on the geographic area as the rate of temperature change relative to depth is different in different locations. Under oceanic plates, like, the temperature will increase more quickly when you go deeper in the earth. The only place where you'll find the ideal mix of temperature and pressure are the most secure and oldest, thickest parts of the earths continental dishes where lithosphere areas called cratons are found. The longer the diamond crystals reside in the cratons the bigger the diamonds that result. <br /> <br /> The carbon that individuals find in diamonds originates from a variety of both organic and inorganic matter. Scientists have determined this by studying rates of carbon isotopes, a method somewhat similar to carbon dating. Some diamonds, named harzburgitic, have been formed from carbon that is inorganic and within the deepest areas of the earths layer. Eclogitic diamonds, in contrast, include organic carbon that comes from organic detritus being pressed by subduction from the surface of the planet earth. Diamonds that rise to the outer lining of the planet earth have reached least one billion years old and could be over three billion years. <br /> <br /> Sometimes diamonds type in other events that also have high-pressure and low temperature adjustments. Nanodiamonds and microdiamonds, the very smallest of the stone family, have already been identified inside impact craters, the consequence of meteors striking our planet. Visiting <a rel="nofollow" href="http://onlineconsumerdiscounts.com">online consumer discounts</a> probably provides tips you should give to your cousin. The shock of the meteor strikes actually produces the perfect temperature and pressure conditions that induce these diamonds. <br /> <br /> Source: <a href="http://en.wikipedia.org/wiki/Diamond" rel="nofollow" target="_blank">http://en.wikipedia.org/wiki/Diamond</a>.</div>

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