According to Wikipedia, a craton is an "...old and stable part of the continental lithosphere" -- the earth's outermost rocky shell.
Kimberlite pipes, where diamonds are commonly found, are sometimes rooted in cratons.
You can read more by following the link, below.
Cratons are the stable interior parts of continents that have not been affected by significant tectonic activity for prolonged periods. They are typically composed of ancient and hard rocks, providing a stable foundation for the continent. Cratons are important for understanding the geological history and evolution of continents.
Diamonds are typically found in regions with specific geological conditions, such as old volcanic pipes or cratons where the high pressure and temperature necessary for diamond formation can occur. These conditions are not common worldwide, so diamonds are only found in certain areas where these geological processes have taken place.
Kimberlite is typically found in regions with ancient volcanic activity, such as cratons and continental lithosphere. Some common locations include southern Africa, Canada, Australia, and Russia. These regions have preserved the deep mantle source rocks that give rise to kimberlite.
The sequences of sedimentary rocks in cratons are typically thin and are relatively undeformed or gently warped. The sequences in mountain belts, meanwhile, are thick and extensively folded and faulted.
Cratons are stable, rigid blocks of the Earth's crust that are not typically prone to rift or shifting apart. However, under certain tectonic forces or geological processes, cratons can experience minor deformation or fragmentation, resulting in rifts or shifts along their edges. Overall, cratons are known for their stability and strength in the Earth's crust.
Cratons contain the ancient crust of igneous rocks.
In old areas of continental crust called "cratons" in volcanic structures called "kimberlite pipes".
Nothing... diamonds are just one base: carbon.Another AnswerThere are diamonds that contain trace elements that can render colour in the stone. Most diamonds contain at least trace amounts of nitrogen, which gives diamonds a yellow cast: fancy yellow diamonds contain more nitrogen. Boron gives diamonds a blue, or blue-gray cast. And so on.Trace elements that give diamonds colour are not separable from the diamond lattice.
Diamonds are formed from carbon. Some brown diamonds may contain trace amounts of nickel -- otherwise diamonds do not contain metals.
No form of chocolate contains diamonds.
Jewelery can contain real diamonds, and jewelery can contain other gems, including stones meant to look like diamonds.
Since diamonds are most rare, indicator minerals are the only way to predict -- sometimes unsuccessfully -- where a miner might locate diamonds.The pipes are always required, since that's how diamonds are pushed up to the surface from earth's upper mantle, and kimberlite is not the only indicator mineral. (Link, below.)Diamond formation does not occur in the pipes: it occurs in cratons. From Wikipedia:"The correct combination of temperature and pressure is only found in the thick, ancient, and stable parts of continental plates where regions of lithosphere known as cratons exist. Long residence in the cratonic lithosphere allows diamond crystals to grow larger."You can read more about cratons, below.
Cratons are the stable interior parts of continents that have not been affected by significant tectonic activity for prolonged periods. They are typically composed of ancient and hard rocks, providing a stable foundation for the continent. Cratons are important for understanding the geological history and evolution of continents.
Some minerals contain carbon, such as graphite and diamonds, however while they both contain carbon, the diamonds density is far greater.
Kimberlite can contain diamonds.
Both diamonds and coal contain carbon atoms in their crystal structure. Diamonds have a tetrahedral lattice structure, while coal has an amorphous structure.
Diamonds are formed from carbon and contain no ores.