It's a thick mass of ignieous rock that lies under the ocean. Where areas of the ocean floor have been upthrust through tectonic plate movement and mountain formation, oceanic crust can also be found inland.
oceanic and the continental crust
Yes, it is.
The lithosphere is composed of the oceanic and continental crusts.
The rocks that makes up the oceanic crusts, are very dark, relatively thin and highly dense.
Near ocean ridges such as the Atlantic ridge
Both oceanic and continental crusts consist primarily of igneous rock although they both contain some sedimentary rock. Oceanic crust is composed mainly of basaltic rock, while continental crust is composed of granitic rock.
The earth's crust is comprised of the oceanic crust and the continental crust. Bread has the crunchy and the sofy crust.
No subduction doesn't take place when two oceanic crust meet. When two oceanic crusts meet, it is called a divergent boundary. Crustal features vary such as one like mid-ocean rdges. Subducting takes place when an OCEANIC and CONTINENTAL plate meet not when two oceanic plates meet.
Oceanic and Continental crusts are alike because they both shift and move and grow. They differ by there rock types. Oceanic crust is made up of dense basalt while continental crust is made up of less dense granite.
There is actually a difference between the thickness of the two. The fact is, however, that actual variance of the Earth's crust is larger than the variance between the continental and oceanic crusts. However, here is the data- The Earth's crust is comprised of layers- the continental crusts are between 35-70 km thick while the oceanic crusts are between 5-10 km thick
When two plates carrying oceanic crusts meet at a trench, one plate typically subducts beneath the other due to its higher density. This process can generate volcanic activity, earthquakes, and the formation of deep-sea trenches and volcanic island arcs.
Oceanic-oceanic collision occurs when two tectonic plates carrying oceanic lithosphere collide with each other. This collision often leads to the subduction of one plate beneath the other, resulting in the formation of volcanic island arcs and deep oceanic trenches. The collision can also lead to the formation of new oceanic crust through volcanic activity.