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Is Crust is neither nor destroyed along a transform boundary?

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


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

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


What type of boundary dose not create or destroy crust?

transform boundary


WHAT TYPE OF BOUNDARY NEITHER NOR DESTROYS OCEANIC CRUST?

Transform boundary.


Is a new oceanic crust formed at a transform fault boundary?

No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.


What type of boundary neither creates nor destroys oceanic crust?

Transform boundary.


Is the crust destroyed or formed in transform boundary?

Niether. At a transform boundary, plates slide past each other, and crust is conserved.


What type of plate boundary does not create or destroy crust?

A transform plate boundary does not create or destroy crust. Instead, adjacent plates slide horizontally past each other. This movement can cause earthquakes along the boundary without significantly changing the amount of crust.


What happen when crust slides past each other?

its called a transform boundary


Is crust neither created nor destroyed along a transform boundry?

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.


A fault generally occurs at a transform boundary?

A strike-slip fault generally occurs at a transform boundary


What boundary has crust neither destroyed nor formed?

The boundary where crust is neither destroyed nor formed is called a transform boundary. At transform boundaries, tectonic plates slide past one another horizontally, leading to significant friction and earthquakes. An example of this type of boundary is the San Andreas Fault in California. These boundaries are characterized by lateral movement rather than the creation or subduction of crust.