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

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WHAT TYPE OF BOUNDARY NEITHER NOR DESTROYS OCEANIC CRUST?

Transform boundary.


What type of boundary neither creates nor destroys oceanic crust?

Transform boundary.


Which feature is commonly formed at a plate boundary where oceanic crust converges with continental crust?

A deep ocean trench is commonly formed at a plate boundary where oceanic crust converges with continental crust. The oceanic crust is denser and is forced beneath the lighter continental crust, creating a deep trench.


Is the crust formed or destroyed at a sliding boundary?

At convergent boundaries are boundaries the crust is destroyed by subduction of oceanic crust underneath continental crust or other oceanic crust.


Is the crust formed or destroyed at the sliding boundary?

At convergent boundaries are boundaries the crust is destroyed by subduction of oceanic crust underneath continental crust or other oceanic crust.


Is the crust destroyed or formed in transform boundary?

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


A fault generally occurs at a transform boundary?

A strike-slip fault generally occurs at a transform boundary


Is a new ocean crust formed at a divergent boundary?

because the molten rock cools in the water and forms a oceanic crust


What type of boundary oceanic crust?

Convergent boundary.


The margin of a continent is the boundary between continental crust and?

oceanic crust


Where is oceanic crust created?

New oceanic crust is created at the mid-oceanic ridges, a divergent plate boundary.


What is continental and oceanic crust?

Continental crust is the thicker, less dense, and older type of crust found beneath continents, primarily composed of granite and sedimentary rock. Oceanic crust is the thinner, more dense, and younger type of crust located beneath oceans, primarily composed of basalt. The boundary between continental and oceanic crust is known as the continental-oceanic crust boundary.