The crust is the Ocean floor. There is Oceanic Crust, And then There is Continental Crust.
The name of the crust beneath the oceans is called "oceanic crust." It is thinner and younger than continental crust and primarily composed of basaltic rocks.
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
Continents are made up of lighter, less dense rock types such as granite and sedimentary rocks, which are usually thicker and less dense than oceanic crust. The ocean floor, on the other hand, is composed mostly of basaltic rock that is denser and thinner than continental crust. Additionally, the ocean floor includes features such as seamounts, ridges, trenches, and abyssal plains formed by various geological processes like seafloor spreading and subduction.
On average, continents are older than ocean basins. Due to the action of plate tectonics, ocean crust is being formed and destroyed continuously. The oldest oceanic crust is about 200 million years old, whereas continents, which are less dense than oceanic crust and tend not to be subducted into the mantle, can be more than 3,000 million years old in places.
Compared to ocean crust near deep-sea trenches, crust near ocean ridges is generally younger, thinner, and hotter. Ocean ridges are sites of active seafloor spreading where magma rises to create new crust, while deep-sea trenches are associated with subduction, where older, denser crust is pulled back into the mantle. As a result, the crust at ocean ridges is also less dense and more buoyant than the crust found near trenches.
The ocean floor is mainly composed of basaltic crust known as oceanic crust. This crust is thinner and denser than continental crust and is formed through volcanic activity at mid-ocean ridges.
It is not. The oceanic crust is thinner than the continental crust!
Approximately 60% of the ocean floor is made up of oceanic crust. Oceanic crust is typically thinner and denser than continental crust, and it forms at mid-ocean ridges through volcanic activity.
The portion of Earth's crust that lies beneath the ocean floor is called oceanic crust. It is thinner and denser than continental crust, primarily composed of basaltic rocks, and formed at mid-ocean ridges through volcanic activity.
The crust under the ocean floor is thinner than the crust under mountain....if thats what your asking....hope it helped!
Oceanic crust is thinner and denser than continental crust.
The Oceanic Crust close to the Mid Ocean Ridge is thinner than that Oceanic Crust far away from the ridge. This is due to tensional forces, as a result of crustal expansion and rock fracturing during the formation of the ridge.the oceanic crust is thinner
It is not. The oceanic crust is thinner than the continental crust!
The crust beneath the ocean is called oceanic crust. It is thinner and younger than continental crust, primarily composed of basaltic rock formed at mid-ocean ridges through volcanic activity.
The crust is much thinner than the mantle.
The crust is much thinner than the mantle.
Crust under the oceans is called oceanic crust.