Craton refers to the stable interior portion of a continent. It is composed of ancient crystalline basement rock, containing both shields and platforms.
A craton
Eastern Canada.
buried beneath other rocks
A craton is 'an old and stable part of the lithosphere' -- the earth's crust. One class of inclusions in the formation of the earth's crust when subductions of crust were folded into the deep, kimberlite diamond areas that lie about 150-450 K below the surface. Diamonds as we know them are exploded to the earth's surface through kimberlite pipes, which are carrot shaped and widest at the surface. Although not all kimberlite pipes are sources for diamonds, most diamonds are found in areas where kimberlite pipes occur.
As material is removed from mountains by erosion, the range floats upward to regain its isostatic balance. This process can be thought of as "the pull of erosion." As the mountains wear down to a low plain, erosion becomes virtually ineffective and the now this crust achieves isostatic balance; the former mountain belt becomes part of the craton.
John Craton was born in 1953.
The relatively stable interior portion of a continent is a craton.
Platforms and shields together make up cratons. The shield is the part of the craton that is exposed at Earth's surface and the platform is the part of the craton that is covered by sedimentary strata.
The stable core of a continent is the old, interior portion that has not experienced significant tectonic activity such as mountain-building or rifting for a long time. It consists of ancient, stable landmasses with low seismic activity and often includes cratons - the oldest and most rigid parts of a continent's lithosphere.
A craton
The North American Craton.
Eastern Canada.
Yes.
Sexy Suz's birth name is Susan Craton.
Ricky Acker's birth name is Richard Craton Acker.
An aulacogen is a tectonic trough on a craton which is formed as the failed arm of a triple-rift junction.
The crust beneath a continent, also known as the continental shield, is a relatively stable region in the interior of a continent. This region is characterized by old and stable geological features like cratons and shields, which have not experienced significant tectonic activity for millions of years.