Diamonds Unearthed

In the first installment of a multi-part series, Smithsonian diamond expert Jeffrey Post, curator of the National Gem and Mineral Collection, explains how the rare crystals form

  • By Cate Lineberry
  • Smithsonian magazine, December 2006, Subscribe
View More Photos »
the hope diamond Jeweler Harry Winston donated the famous Hope Diamond—the largest-known deep blue diamond in the world—to the Smithsonian Institution in 1958. It arrived in a plain brown package by registered mail, insured for one million dollars. Surrounded by 16 white pear-shaped and cushion-cut diamonds and hanging from a chain with 45 diamonds, the rare gem attracts 6 million visitors a year to the Natural History Museum.

Chip Clark

 

Article Tools

 
  • Comments (14)
  • Font
    		•
  • Email
    		•
  • RSS
    		•
  • Print
    		•
  • Single Page
    		•

    Photo Gallery

    the hope diamond

    Diamonds Unearthed

    Explore more photos from the story

    More from Smithsonian.com

    How are diamonds formed?

    Diamonds are formed deep within the Earth about 100 miles or so below the surface in the upper mantle. Obviously in that part of the Earth it's very hot. There's a lot of pressure, the weight of the overlying rock bearing down, so that combination of high temperature and high pressure is what's necessary to grow diamond crystals in the Earth. As far as we know, all diamonds that formed in the Earth formed under those kinds of conditions and, of course, that's a part of the Earth we can't directly sample. We don't have any way of drilling to that depth or any other way of traveling down to the upper mantle of the Earth.

    How do diamonds travel to the surface of the Earth?

    The diamonds that we see at the surface are ones then that are brought to the surface by a very deep-seated volcanic eruption. It's a very special kind of eruption, thought to be quite violent, that occurred a long time ago in the Earth's history. We haven't seen such eruptions in recent times. They were probably at a time when the earth was hotter, and that's probably why those eruptions were more deeply rooted. These eruptions then carried the already-formed diamonds from the upper mantle to the surface of the Earth. When the eruption reached the surface it built up a mound of volcanic material that eventually cooled, and the diamonds are contained within that. These are the so-called Kimberlites that are typically the sources of many of the world's mined diamonds.

    One of the things we know, therefore, about any diamonds that were brought to the surface is that the process of the Kimberlite eruption bringing the diamonds from the upper mantle to the surface of the Earth had to happen very quickly, because if they were traveling too long and too slowly they would have literally turned into graphite along the way. And so by moving quickly they essentially got locked into place into the diamond structure. Once the diamonds have been brought from high temperature to low temperature very quickly—and by quickly, we mean in a matter of hours—these eruptions, these Kimberlite pipes moving to the surface, may have been traveling at rates of 20 to 30 miles per hour. Once the diamonds are brought to the surface and cooled relatively quickly, those carbon atoms are locked into place and there's just not enough energy to now start rearranging them into graphite.

    What is carbon's role in forming diamonds?

    Diamonds are made of carbon so they form as carbon atoms under a high temperature and pressure; they bond together to start growing crystals. Because of the temperature and pressure, under these conditions, carbon atoms will bond to each other in this very strong type of bonding where each carbon atom is bonded to four other carbon atoms. That's why a diamond is such a hard material because you have each carbon atom participating in four of these very strong covalent bonds that form between carbon atoms. So as a result you get this hard material. Again where the carbon is coming from, how quickly they're growing, those are all still open questions, but obviously the conditions are such that you've got some group of carbon atoms that are in close enough proximity that they start to bond. As other carbon atoms move into the vicinity they will attach on. That's the way any crystal grows. It's the process of atoms locking into place that produces this repeating network, this structure of carbon atoms, that eventually grows large enough that it produces crystals that we can see. Each of these crystals, each diamond, one carat diamond, represents literally billions and billions of carbon atoms that all had to lock into place to form this very orderly crystalline structure.

    You mentioned that scientists don't know where the carbon comes from. What are some possible sources?

    In some cases, the carbon seems to have originated within the mantle of the Earth, so carbon that was already in the Earth. In other cases, there's evidence very curiously to suggest that the carbon may have originated near the surface of the Earth. The thinking there is that this carbon could have literally been carbon that was part of carbonate sediments or animals, plants, shells, whatever, that was carried down into the upper mantle of the Earth by the plate tectonics mechanism called subduction.

    How long does it take diamonds to form?


    How are diamonds formed?

    Diamonds are formed deep within the Earth about 100 miles or so below the surface in the upper mantle. Obviously in that part of the Earth it's very hot. There's a lot of pressure, the weight of the overlying rock bearing down, so that combination of high temperature and high pressure is what's necessary to grow diamond crystals in the Earth. As far as we know, all diamonds that formed in the Earth formed under those kinds of conditions and, of course, that's a part of the Earth we can't directly sample. We don't have any way of drilling to that depth or any other way of traveling down to the upper mantle of the Earth.

    How do diamonds travel to the surface of the Earth?

    The diamonds that we see at the surface are ones then that are brought to the surface by a very deep-seated volcanic eruption. It's a very special kind of eruption, thought to be quite violent, that occurred a long time ago in the Earth's history. We haven't seen such eruptions in recent times. They were probably at a time when the earth was hotter, and that's probably why those eruptions were more deeply rooted. These eruptions then carried the already-formed diamonds from the upper mantle to the surface of the Earth. When the eruption reached the surface it built up a mound of volcanic material that eventually cooled, and the diamonds are contained within that. These are the so-called Kimberlites that are typically the sources of many of the world's mined diamonds.

    One of the things we know, therefore, about any diamonds that were brought to the surface is that the process of the Kimberlite eruption bringing the diamonds from the upper mantle to the surface of the Earth had to happen very quickly, because if they were traveling too long and too slowly they would have literally turned into graphite along the way. And so by moving quickly they essentially got locked into place into the diamond structure. Once the diamonds have been brought from high temperature to low temperature very quickly—and by quickly, we mean in a matter of hours—these eruptions, these Kimberlite pipes moving to the surface, may have been traveling at rates of 20 to 30 miles per hour. Once the diamonds are brought to the surface and cooled relatively quickly, those carbon atoms are locked into place and there's just not enough energy to now start rearranging them into graphite.

    What is carbon's role in forming diamonds?

    Diamonds are made of carbon so they form as carbon atoms under a high temperature and pressure; they bond together to start growing crystals. Because of the temperature and pressure, under these conditions, carbon atoms will bond to each other in this very strong type of bonding where each carbon atom is bonded to four other carbon atoms. That's why a diamond is such a hard material because you have each carbon atom participating in four of these very strong covalent bonds that form between carbon atoms. So as a result you get this hard material. Again where the carbon is coming from, how quickly they're growing, those are all still open questions, but obviously the conditions are such that you've got some group of carbon atoms that are in close enough proximity that they start to bond. As other carbon atoms move into the vicinity they will attach on. That's the way any crystal grows. It's the process of atoms locking into place that produces this repeating network, this structure of carbon atoms, that eventually grows large enough that it produces crystals that we can see. Each of these crystals, each diamond, one carat diamond, represents literally billions and billions of carbon atoms that all had to lock into place to form this very orderly crystalline structure.

    You mentioned that scientists don't know where the carbon comes from. What are some possible sources?

    In some cases, the carbon seems to have originated within the mantle of the Earth, so carbon that was already in the Earth. In other cases, there's evidence very curiously to suggest that the carbon may have originated near the surface of the Earth. The thinking there is that this carbon could have literally been carbon that was part of carbonate sediments or animals, plants, shells, whatever, that was carried down into the upper mantle of the Earth by the plate tectonics mechanism called subduction.

    How long does it take diamonds to form?

    We really don't know how long it takes. There have been attempts to try to date inclusions in different parts of diamonds, and those have largely been unsuccessful. It may be that diamonds form over periods as short a time as days, weeks, months to millions of years. Typically, as with many crystals that grow on the Earth, it's not a continuous process. The diamonds may start to grow and then there may be an interruption for some reason – a change in conditions, temperature, pressure, source of carbon, whatever—and they could sit for millions, hundreds of million of years, and then start growing again. That's part of the problem of trying to put some sort of a growth period on them; things don't always occur continuously in the Earth.

    We can grow diamonds in the lab and we can simulate conditions there. But there are things we have to do to grow diamonds in the laboratory that aren't obvious as to how it happens in the Earth. In the laboratory, they're typically grown, but there's some catalyst. Some metals are often added to cause the diamonds to grow, but these same catalysts are not observed in the diamonds from the upper mantle of the Earth.

    How old then are diamonds?

    All diamonds, as far as we know, are quite old in the Earth. Most diamond formation probably took place in the Earth in the first couple billion years of the Earth's history. There are diamond deposits that have been discovered that are younger—the rock itself, the Kimberlite, is maybe just tens of hundreds of millions of years old. The way they date diamonds is typically looking at inclusions of other minerals in the diamond that can be radioactively dated. The diamonds themselves can't be dated. But if the mineral inclusions contain certain elements like potassium and things that can be used in a radioactive dating scheme, then by dating the inclusion in the diamond you get some sense of the age of the diamond itself. And those dates always suggest the diamonds are quite old. At least hundreds of millions of years old, but in most cases billions of years old, anywhere from one to three billion years old, a time when the earth was probably hotter than it is today and so conditions were perhaps more appropriate for diamond growth.

    How old is the famous Hope Diamond on display at Smithsonian's Natural History Museum?

    The Hope diamond is at least a billion years old. You don't see the original rock that carried the diamonds to the surface, but they have found some Kimberlites in India that do have evidence of diamonds in them. Those Kimberlites date to at least a billion years old. So that suggests the Hope diamond and similar diamonds found in India were brought to the surface at least a billion years ago and perhaps longer ago. So we're comfortable saying that the Hope Diamond is at least a billion years old. When you look at the age spread of most other diamonds, it's probably much older that that.

    What makes the Hope Diamond so unusual?

    Its size and color make it very unusual. When you think of the history of people mining diamonds, only one diamond has ever been found that has produced a dark-blue diamond the size and quality of the Hope Diamond. That gives you some sense of just how unusual and how remarkable it is. Again, I've always argued that it's as remarkable as a natural history object, as a product of the Earth, as it is a human-cut gemstone. Most of the time when people write about the Hope Diamond they start with, "Well it was found in India." Part of the point I always try to make to people is really the story began a lot sooner. Many diamonds don't ever get to that point because they just didn't survive all these things that had to have happened.

    In part two, learn about colored diamonds, how scientists are growing synthetic versions in the lab, and global efforts to curb the sale of conflict diamonds. In the final installment of this three-part series, discover the fascinating stories behind the Smithsonian's collection.


    1 2 Next »

        Subscribe now for more of Smithsonian's coverage on history, science and nature.



    Digg
     
    Comments (14)

    This is a great article, it really helped me with my science project.

    Posted by kristen on November 3,2011 | 07:43 PM

    NOTE:- South African diamonds were formed by the Vredefort impact meteorite that carried carbon from coal deposits down to earth's mantle - very high impact, speed and pressure (70 million megaton impact) - this also released the Platinum & others (PGMs) from down below in the so called Lowveld cradle all the way from Parys to Pieterersburg (Polokwane). Many tiny volcanoes are evident especially near the town of Brits.

    Now we know...

    Posted by WWJD on April 3,2011 | 03:23 PM

    the diamond is cool

    Posted by austin on April 9,2010 | 03:46 PM

    this site is so cool because i like diamonds

    Posted by De'Carlos Lyons on October 22,2009 | 09:07 AM

    hi i just want to say that i found your website very interesting, i am currently doing a school assement on diamonds. thanx so much!

    Posted by Gabrielle on May 18,2009 | 04:06 AM

    I found this website very interesting, and am using it for a school project. I am also looking for information on * Industrial diamonds and how it works
    * mining of diamonds - process today
    * and how diamonds are cut etc.
    Thanks Louisa

    Posted by Louisa Pretorius on May 14,2009 | 10:30 AM

    This was so interesting!. I did not know that much about diamonds until I had to search this for school project just like Enya (she is a friend from school). I thought diamonds are just found in mines around the world. Thanks a Lot!

    Posted by Benjamin Vazirani on April 6,2009 | 10:08 PM

    I was doing research for a school project about diamonds. When I Blackle searched it (blackle is like google but saves energy! 2 google searches are is as much enery as boiling acup of tea!!! go to www.blackle.com) and found this it helped SOOOO much!!! thanks guys!!!

    Posted by Enya on April 5,2009 | 09:35 PM

    aww that necklace looks like the one on titanic!

    Posted by Genesse Raygoza on March 5,2009 | 06:31 PM

    I really enjoyed your article on the diamond supposibly found at the crater of diamonds state park, I,m planning a trip there in April with the hopes of finding that large special diamond myself, this is the first trip I,ve ever planned and I cant wait until we get there, I,m not surprised that the amount of visitors has trippled in the past few years.I,m a hugh diamond lover, I need just that one special diamond and I,ll have a diamond ring for everyone of my fingers so maybe its there just waiting for me to find, I also consider them to be good luck charms and also named my cats diamond and jewel. Teresa

    Posted by teresa on January 14,2009 | 09:33 PM

    what parts of arkansas are the diamond what city,Thank You F. mora Sr.

    Posted by Felipe Mora on January 14,2009 | 08:48 PM

    Kimberlites aren't the only volcanic rock diamonds are found in. Lamprophyre dikes (made of lamproite rock), like kimberlite dikes, also deliver diamonds from "cratons" the roots of continents. Either way, the theory goes, the diamond does not form in these volcanic rocks; it forms elsewhere but is brought to the surface, as the molten material picks them up, in the molten material as xenocrysts. Also, the article incorrectly links biogenic carbon with diamonds. The carbon of diamonds is most likely not derived from ancient life but from sources deep within the Earth. Also, the intense shock of a meteor impact can form small diamonds although not every meteor crater will yield diamonds. But can we be absolutely certain about any of the science behind diamond formation and transport? Well, not really. It's still guesswork. Highly educated guesswork, but still guesswork.

    Posted by LV on November 26,2008 | 10:26 AM

    We just got to go to the museum and see the Hope diamond and all the other rare jewels. Everyone should have a chance to go there, but this sight is the next best thing! Thanks

    Posted by BTB on May 12,2008 | 12:45 PM

    I'm doing a report on the Hope Diamond! It has like 350 years of History to cover

    Posted by Jonathan on April 24,2008 | 11:16 AM

    Post a Comment


    Name: (required)

    Email: (required)

    Comment:

    Comments are moderated, and will not appear until Smithsonian.com has approved them. Smithsonian reserves the right not to post any comments that are unlawful, threatening, offensive, defamatory, invasive of a person's privacy, inappropriate, confidential or proprietary, political messages, product endorsements, or other content that might otherwise violate any laws or policies.



    Advertisement


    Advertisement

    Follow Us






    First Name
    Last Name
    Address 1
    Address 2
    City
    State   Zip
    Email

    Smithsonian Store

    Smithsonian Journeys