The oldest continental crust is found in large, stable areas with little seismic/volcanic activity found in the centre of continents, called Cratons. Examples of these are Yilgarn Craton in Australia, and the Kaapvaal Craton in South Africa. The oldest rocks found within these cratons can be up to 3.8 billion years old (3,800 million).
However, because the forces of erosion and deposition are always at work creating new rocks, continental crust also contains much younger rocks - some only a few hundred thousand years old.
In short, there is no specific age for continental crust, and unlike oceanic crust that is created and destroyed at a fairly constant rate, continental crust is less dense and thus doesn't undergo subduction at plate boundaries. Less "recycling" means older rocks are more likely to survive.
Continental plate.
It is oceanic
Continental plate.
It's because the oceanic plate is more dense than the continental plate.
the african plate is continental
the african plate is continental
It subducts under the continental plate because the oceanic plate is denser.
the recent earthquake in japan is an of the movement plate techtonics
The oceanic plate must be more dense than the continental plate for this to happen.
the oceanic plate is more dense and subducts, or goes below, the continental plate.
No. It subducts under the continental plate.
It will subduct under the less dense continental plate.