According to the theory of plate tectonics, how do two plates interact to form coastal volcanic ranges?

A.
A continental plate slides along an oceanic plate at a convergent boundary.

B.
A continental plate collides with another continental plate at a convergent boundary.

C.
An oceanic plate sinks beneath another oceanic plate at a convergent boundary.

D.
An oceanic plate sinks beneath a continental plate at a convergent boundary.**

I think it might be D

I think it is D too.

Prty sre its d

The correct answer is D. An oceanic plate sinks beneath a continental plate at a convergent boundary.

To understand why this option is correct, we need to explore the theory of plate tectonics and the different types of plate boundaries.

The theory of plate tectonics states that the Earth's lithosphere (made up of rigid plates) is divided into several large and small pieces that are constantly moving. These plates interact with each other at their boundaries, which fall into three main types: convergent boundaries, divergent boundaries, and transform boundaries.

Convergent boundaries are areas where two plates collide or come together. They can form various types of geological features depending on the types of plates involved. One common occurrence at convergent boundaries is the subduction of one plate beneath another.

In the case of coastal volcanic ranges, we see the interaction between an oceanic plate and a continental plate at a convergent boundary. As the oceanic plate, which is denser, collides with the less dense continental plate, it starts to sink or subduct beneath the continental plate.

As the oceanic plate sinks deeper into the Earth's mantle, it begins to heat up and undergoes melting. This melted material, called magma, is less dense than the surrounding rocks and rises towards the surface. Eventually, the magma reaches the surface and erupts, forming volcanoes along the coast.

Therefore, option D - An oceanic plate sinks beneath a continental plate at a convergent boundary - is the correct choice for how two plates interact to form coastal volcanic ranges according to the theory of plate tectonics.