Plate tectonic movement and subduction zones.
Oceanic
Oceanic and continental combined is approximately 25 miles.
Tectonic plates which may be either oceanic or continental in nature.
Earth's oceanic crust is thinner, denser, and younger than Earth's continental crust. It is primarily composed of basaltic rock, whereas continental crust is made up of less dense granitic rock. Oceanic crust is constantly being formed at mid-ocean ridges and destroyed at subduction zones.
Oceanic crust is denser than continental crust. Oceanic crust has a density of about 3 g/cm^3, while continental crust has a lower density of about 2.7 g/cm^3.
a section of both continental and oceanic lithosphere
a section of both continental and oceanic lithosphere
The largest layer of Earth's surface is the crust, which is divided into oceanic and continental crust. The continental crust is thicker and less dense than the oceanic crust, covering about 40% of the Earth's surface.
Oceanic crust is denser than continental crust, it floats lower in earths mantle.
PLATE TECTONICS is the study of the movement of the earths continental plates
These are individual broken slabs of gigantic masses, that makes up the earths crust and are capable of floatational movement over the weak, plastic, hot and highly molten portion of the mantle called the asthenosphere.
The Earths Crust can be divided between Oceanic Crust and Continental Crust. Oceanic and Continental Crust are quiet different. The thickness of oceanic crust is between 5km and 10km. It is made of mainly basalt, grabbo and diabise. The thickness of continental crust is between 30km and 50km. It is made up of lighter rocks such as granite.