the deep ocean basin
The two types of crust that make up the continents and ocean are the continental crust and the oceanic crust.
The oceanic plate is thin, dense, and makes up the ocean floor. The continental plate is less-dense, thick, and make up the continents.
Primarily lime stone.
Basalt is the most common rock that makes up oceanic crust. It is formed from solidified lava from volcanic eruptions along mid-ocean ridges.
Basalt is the iron-rich volcanic rock that makes up much of the ocean floor. It forms from the cooling and solidification of magma that erupts through underwater volcanic activity, such as mid-ocean ridges. Basalt is a key component of Earth's oceanic crust.
The two types of crust that make up the continents and ocean are the continental crust and the oceanic crust.
the deep ocean basin
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 process that makes new crust when the sea floor moves apart and magma rises up is called seafloor spreading. Magma from the mantle rises to the surface at mid-ocean ridges, cools, and solidifies to form new crust as the tectonic plates move apart. This process contributes to the continuous growth of the seafloor and the expansion of the ocean basins.
Crust is made up of mainly granite, a felsic rock wit a lower density than basalt, what makes up the ocean's crust, thus why the continental crust rises up compared to ocean crust.
The oceanic crust is the part of the earth's crust that is below the ocean. The rock that makes up the oceanic crust is about 200 million years old.
Convergence supports the theory of seafloor spreading. Samples of the deep ocean floor are evidence of seafloor spreading because the basaltic oceanic crust and overlapping sediment become younger as the mid-ocean ridge is approached. Also, the rock that makes up the floor of the ocean is younger than the continents.
basalt
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.
1. The Oceanic crust is dense while the Continental crust is relatively lighter. 2. The Oceanic crust consists of Silicon and Magnessium, while the Continental crust has Silicon and Alluminium. 3. The Oceanic crust is thin, while the Continental crust is thick. 4. The Oceanic crust makes up the ocean floor, while the Continental crust carries the continents.
Primarily lime stone.