It is created at mid-oceanic ridges (divergent boundaries) and it is destroyed at subduction zones (convergent boundary between oceanic crust and continental crust).
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.
near ocean trenches.
Crust is neither formed nor destroyed at transform plate boundaries. At these boundaries, tectonic plates slide past each other horizontally, resulting in earthquakes and faults but no new crust is created or destroyed.
At divergent plate boundaries, crust is formed through the process of seafloor spreading. At convergent plate boundaries, crust is often destroyed through subduction, where one plate is forced beneath another into the mantle. At transform plate boundaries, crust is neither created nor destroyed, as the plates slide past each other horizontally.
Crust is neither created nor destroyed along a transform boundary. Transform boundaries are characterized by horizontal displacement of crustal blocks, where tectonic plates slide past each other. This movement does not involve the production or destruction of crust, but rather leads to earthquakes due to the friction and stress along the boundary.
The Earth's crust is destroyed when subduction occurs.
it's neither created or destroyed
the shifting of earths crust
from the earths crust pushing together
No crust is created when a transform boundary pulls away from each other.
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.
The Earth's crust is destroyed when subduction occurs.
near ocean trenches.
Crust is neither formed nor destroyed at transform plate boundaries. At these boundaries, tectonic plates slide past each other horizontally, resulting in earthquakes and faults but no new crust is created or destroyed.
The Earths crust is approximately 650 km deep.
At divergent plate boundaries, crust is formed through the process of seafloor spreading. At convergent plate boundaries, crust is often destroyed through subduction, where one plate is forced beneath another into the mantle. At transform plate boundaries, crust is neither created nor destroyed, as the plates slide past each other horizontally.
Earth's crust is neither created nor destroyed because of the process of plate tectonics. The crust is continuously recycled through processes like subduction and seafloor spreading, where old crust is consumed and new crust is formed. This dynamic balance ensures that the total amount of crust remains relatively constant over geological time scales.