no
Because oceanic crust is gradually being created and subducted, it is newer than continental crust.
Continental crust "floats" on the denser mantle and resists being pulled into the earth where it could be melted into new rock. Oceanic crust gets subducted and "recycled" more often.
Oceanic lithosphere is recycled by subduction on timescales of about 200 - 300 million years depending on rate of sea floor spreading. Continental lithosphere does not undergo subduction due to its low density. Therefore, the continental lithosphere is older than oceanic lithosphere.
No. Ocean floor rocks are younger than continental rocks.
Yes. Oceanic crust is rarely over 200 million years in age. The oldest continental crustal rocks are around 4 billion years in age.
no
no. false
No continental lithosphere contains more felsic rocks than oceanic lithosphere.
The density of the continental (granitic) lithosphere is lower than oceanic (basaltic) lithosphere. Consequently, due to buoyancy, the continental crust rides above the oceanic lithosphere and thus is not subducted. However, it is thought that pieces of the continental lithosphere break off and are subducted along with the oceanic lithosphere.
Continental crust is generally lighter than oceanic crust.
Continental plates are thicker and less dense. Continental plates are mainly granitic in composition. Oceanic plates are mainly basaltic in composition. The rock of continental plates is on average, much older than the rock of the oceanic plates. The oceanic plate underlies the oceans, and the continental plate makes up the land masses. Continental plates do not subduct at convergent plate boundaries.
The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere. The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
No continental lithosphere contains more felsic rocks than oceanic lithosphere.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
The density of the continental (granitic) lithosphere is lower than oceanic (basaltic) lithosphere. Consequently, due to buoyancy, the continental crust rides above the oceanic lithosphere and thus is not subducted. However, it is thought that pieces of the continental lithosphere break off and are subducted along with the oceanic lithosphere.
Continental lithosphere is thicker and less dense than oceanic lithosphere. Continental crust is primarily composed of granitic rock while oceanic crust is composed primarily of basaltic rock.
Continental crust is generally lighter than oceanic crust.
No, the oceanic crust is denser. That's why the land areas "float" so much higher than the ocean bedrock.
Continental plates are lighter (less dense) than oceanic plates.
Continental plates are thicker and less dense. Continental plates are mainly granitic in composition. Oceanic plates are mainly basaltic in composition. The rock of continental plates is on average, much older than the rock of the oceanic plates. The oceanic plate underlies the oceans, and the continental plate makes up the land masses. Continental plates do not subduct at convergent plate boundaries.
Continental plates are lighter than oceanic plates
The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere. The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere.