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What type of boundary neither creates 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 NOR DESTROYS OCEANIC CRUST?

Transform boundary.


What type of boundary destroys oceanic crust?

Convergent boundary.


What creates an ocean trench?

A convergent boundary between a continental plate and an oceanic plate


Which plate boundary destroys crust?

Crust is destroyed at the convergent plate boundary. This is usually between the oceanic and continental plates. This is where subduction of the more dense crust occurs.


Which convergent boundary that does not have a subduction zone?

A convergent boundary that does not have a subduction zone is a continental-continental convergent boundary. At this type of boundary, two continental plates collide and crumple, leading to the formation of mountain ranges, such as the Himalayas. Since both plates are buoyant and primarily composed of continental crust, neither plate is forced beneath the other, unlike in oceanic-continental or oceanic-oceanic boundaries.


What is an example of convergent boundary oceanic-oceanic?

an oceanic trench


What is an example of a oceanic oceanic convergent boundary?

an oceanic trench


What type of boundary forms when an oceanic plate is pushed under a continental plate?

A convergent boundary forms when an oceanic plate is pushed under a continental plate. This process, known as subduction, can result in the formation of deep ocean trenches, volcanic arcs, and earthquakes.


What are the types of convergent boundary?

There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.


What happens between oceanic and oceanic plates in an convergent boundary?

At a convergent boundary between two oceanic plates, one plate is subducted beneath the other due to differences in density. This subduction creates a trench in the ocean floor and can lead to volcanic island arcs as magma rises to the surface. The intense pressure and friction at this boundary can also cause earthquakes. Over time, this process contributes to the recycling of oceanic crust into the mantle.