A craton is a stable portion of a continental crust that forms the core of a continent, similar to how roots anchor and support a plant. Cratons are the oldest and most stable parts of continents, serving as the foundation upon which the rest of the continent is built, akin to how roots provide stability and nutrients to a plant. Just as roots extend deep into the ground to support and nourish the plant above, cratons extend deep into the Earth's mantle to support and stabilize the continents.
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.
Yes, Continental shields and stable platforms are both part of a craton, which is the ancient, stable interior region of a continent. Shields are the exposed areas of a craton, while stable platforms are the surrounding flat regions. Together, they form the stable interior core of a continent.
The Dharwar Craton in southern India contains some of the oldest rocks in India, which date back to around 3.1 - 3.4 billion years. These rocks are predominantly found in areas like Karnataka and Andhra Pradesh.
Evidence supporting the theory of the supercontinent Pangaea includes the jigsaw-like fit of continents, similarities in rock formations and mountain ranges across continents that align when continents are brought together, distribution of fossils of identical species across distant continents, and similarities in ancient climates and geological records found on separate continents. These pieces of evidence work together to suggest that the current continents were once part of a single landmass.
The shape of continents is the result of tectonic plate movement over millions of years. This movement causes landmasses to drift apart, collide, or slide alongside each other, shaping the continents as we see them today. Erosion and other natural forces also play a role in shaping the landforms on the continents.
they both have .red roots .they both can grow up to 27 ft .
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 Canadian Shield is an ancient and stable geological formation, characteristic of a craton. It consists of some of the Earth's oldest rocks and has remained largely unchanged for billions of years, making it a prime example of a craton - a large, stable portion of the continental lithosphere.
the earths continents are the same ..
The North American Craton.
Yes, Continental shields and stable platforms are both part of a craton, which is the ancient, stable interior region of a continent. Shields are the exposed areas of a craton, while stable platforms are the surrounding flat regions. Together, they form the stable interior core of a continent.
The continents look like that because they use to be a SUPER-CONTINENT called PANGAEA.
The oldest and most stable part of a continent is usually the craton, which is a large area of exposed ancient rocks that have not undergone significant tectonic activity for millions of years. Cratons are found in the interior regions of continents and provide a stable foundation for the continent's geology.
Sexy Suz's birth name is Susan Craton.
The Canadian Shield is a large part of the North American craton. It is a stable geological region made up of ancient rocks that have remained relatively undisturbed for billions of years.