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It is created at mid-oceanic ridges (divergent boundaries) and it is destroyed at subduction zones (convergent boundary between oceanic crust and continental crust).

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Related Questions

When is earths Crust destroyed?

The Earth's crust is destroyed when subduction occurs.


Is the earth's crust destroyed or created along a sliding boundary?

it's neither created or destroyed


How do tidal waves get created?

the shifting of earths crust


How were volcanoes created in California?

from the earths crust pushing together


Is Crust is neither created nor destroyed along a transform boundary?

No crust is created when a transform boundary pulls away from each other.


Compared to earths continental crust earths oceanic crust is?

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.


When Crust is destroyed.?

The Earth's crust is destroyed when subduction occurs.


Is crust being destroyed or created?

near ocean trenches.


Where is crust neither formed nor destroyed?

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.


What is the size of the earths crust?

The Earths crust is approximately 650 km deep.


Is crust formed or destroyed at each type of plate boundary?

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.


Why is Earth's crust neither created or destroyed?

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.