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The heavier (usually older and cooler hence more dense) oceanic crust normally subducts (is forced under) the younger less dense crust.
The crust contains the ocean floor and also the continents on Earth.
The least dense layer of the earth is the Crust , the mantle is second densest , whereas the core is the most dense layer of the earth
Oceanic crust, formed mostly of mafic rocks, or sima, is found on the ocean floor.
It becomes more dense as it cools, until its density is greater than the asthenosphere below it.
Trenches are the lowest points on the crust of the Earth, created by the subduction of oceanic crust beneath less dense crust.
oceanic crust
The heavier (usually older and cooler hence more dense) oceanic crust normally subducts (is forced under) the younger less dense crust.
The ocean crust dives below the continental crust due to a collision. This collision involves the two types of crust and since the oceanic crust is denser, it sinks to the bottom while the less dense continental crust rises to the top.
The crust contains the ocean floor and also the continents on Earth.
The youngest oceanic crust can be found near the mid-ocean ridges.
The oceanic plate is thin, dense, and makes up the ocean floor. The continental plate is less-dense, thick, and make up the continents.
The least dense layer of the earth is the Crust , the mantle is second densest , whereas the core is the most dense layer of the earth
It becomes more dense as it cools, until its density is greater than the asthenosphere below it.
It is found at the bottom of the ocean!
Oceanic crust, formed mostly of mafic rocks, or sima, is found on the ocean floor.
It becomes more dense as it cools, until its density is greater than the asthenosphere below it.