|Do diamonds really come from coal?|
Many people believe that diamonds are formed from the metamorphism of coal. That idea continues to be the "how diamonds form" story in many science classrooms.
It's easy to see where the idea came from, though. Diamonds and coal are both, at their base, different forms of the element carbon (C on the periodic table). And yes, pressure is a key part of what turns decaying carbon-based life forms such as plants into coal, as well as what turns carbon into diamonds. But the reality is just a little bit more complex than Superman's super-strength.
First of all, let's look at the chemical compositions of these two forms of carbon. Diamonds are essentially pure carbon formed into a crystalline structure. The rarer, colored diamonds do contain minor impurities (boron, for example, makes diamonds blue, while nitrogen turns them yellow), but those impurities exist on a scale of just one atom in a million.
Another problem with the idea is that coal seams are sedimentary rocks that usually occur as horizontal or nearly horizontal rock units. However, the source rocks of diamonds are vertical pipes filled with igneous rocks.
Beyond that, carbon requires a lot more than pressure to become a diamond. It also requires enormous amounts of heat. In fact, diamonds require a combination of heat (thousands of degrees) and pressure (130,000 atmospheres) that can typically only be found about 90 to 100 miles below the surface of the Earth, deep within the mantle. This heat and pressure work together to allow the carbon to form into the crystalline lattice structure that we know so well. When presented with this heat and pressure, each carbon atom bonds with four other atoms in what is known as a tetrahedral unit. This strong molecular bond provides diamonds with not just their structure but also their classic hardness. That bond would not be possible if impurities were present on anything but a superficial level.
Geologists believe that the diamonds in all of Earth's commercial diamond deposits were formed in the mantle and delivered to the surface by deep-source volcanic eruptions. These eruptions produce the kimberlite and lamproite pipes that are sought after by diamond prospectors. Diamonds weathered and eroded from these eruptive deposits are now contained in the sedimentary (placer) deposits of streams and coastlines.
The formation of natural diamonds requires very high temperatures and pressures. These conditions occur in limited zones of Earth's mantle about 90 miles (150 kilometers) below the surface where temperatures are at least 2000 degrees Fahrenheit (1050 degrees Celsius). This critical temperature-pressure environment for diamond formation and stability is not present globally. Instead it is thought to be present primarily in the mantle beneath the stable interiors of continental plates.
Diamonds formed and stored in these "diamond stability zones" are delivered to Earth's surface during deep-source volcanic eruptions. These eruptions tear out pieces of the mantle and carry them rapidly to the surface. See Location 1 in the diagram at the top of the page. This type of volcanic eruption is extremely rare and has not occurred since scientists have been able to recognize them.
Tiny diamonds have been found in rocks that are thought to have been subducted deep into the mantle by plate tectonic processes - then returned to the surface. Diamond formation in a subducting plate might occur as little as 50 miles (80 kilometers) below the surface and at temperatures as low as 390 degrees Fahrenheit (200 degrees Centigrade). In another study, diamonds from Brazil were found to contain tiny mineral inclusions consistent with the mineralogy of oceanic crust. Others have inclusions that suggest that subducted seawater was involved in their formation.
Is coal involved? Coal is a possible carbon source for this diamond-forming process. However, oceanic plates are more likely candidates for subduction than continental plates because of their higher density. The most likely carbon sources from the subduction of an oceanic plate are carbonate rocks such as limestone, marble, and dolomite, and possibly particles of plant debris in offshore sediments.
Throughout its history, Earth has been repeatedly hit by large asteroids. When these asteroids strike the earth, extreme temperatures and pressures are produced. For example: when a six mile (10 kilometer) wide asteroid strikes the earth, it can be traveling at up to 9 to 12 miles per second (15 to 20 kilometers per second). Upon impact this hypervelocity object would produce an energy burst equivalent to millions of nuclear weapons and temperatures hotter than the sun's surface.
The high temperature and pressure conditions of such an impact are more than adequate to form diamonds. This theory of diamond formation has been supported by the discovery of tiny diamonds around several asteroid impact sites.
The most convincing evidence that coal did not play a role in the formation of most diamonds is a comparison between the age of Earth's diamonds and the age of the earliest land plants.
Since coal is formed from terrestrial plant debris, and the oldest land plants are younger than almost every diamond that has ever been dated, it is easy to conclude that coal did not play a significant role in the formation of Earth's diamonds.
- Erlich, E.I.; Dan Hausel, W. (2002). Diamond Deposits. Society for Mining, Metallurgy, and Exploration. pp. 74-94. ISBN 0873352130.
- American Museum of Natural History (1998). The Nature of Diamonds - Diamonds are Found on Continental Cores. American Museum of Natural History.
- American Museum of Natural History (1998). The Nature of Diamonds - Kimberlite and Lamproite. American Museum of Natural History.
- American Museum of Natural History (1998). The Nature of Diamonds - From Continental Collisions, Meteor Impacts and Star Dust. American Museum of Natural History.