If the plates are moving toward each other from opposite directions, the more dense oceanic plate will subduct in a conveyor belt like operation under the less dense continental plate. Transform plate boundaries occur where plates of any combination grind alongside each other and result in faults and earthquakes.
When two oceanic plates meet, one plate is usually forced beneath the other in a process called subduction. This can lead to the formation of deep ocean trenches and volcanic activity. Earthquakes can also occur along the boundary between the two plates.
Either plates gets subducted which is usually the older plate.
At a convergent boundary where two oceanic plates meet, the denser plate will typically subduct below the less dense plate. The denser plate is usually the older, cooler, and more compacted of the two plates.
When an oceanic to oceanic happens, two oceanic plates converge and one of the plates subducts into a trench. The subducted plate sinks down into the mantle and begins to melt. Molten rock from the plate rises toward the surface and forms a chain of volcanic islands, also called a volcanic island arc, behind the trench in the ocean.
Oceanic plates typically subduct beneath continental plates or other oceanic plates at subduction zones. The denser oceanic plate is forced beneath the less dense continental plate, leading to the formation of features such as deep ocean trenches, volcanic arcs, and earthquakes.
an earth quake happens when two plates meet
they bang
When two oceanic plates meet, one plate is usually forced beneath the other in a process called subduction. This can lead to the formation of deep ocean trenches and volcanic activity. Earthquakes can also occur along the boundary between the two plates.
At plate boundaries.
It makes a mountain.
Oceanic plates are sections of the Earth's lithosphere that form the bedrock beneath the world's oceans. These plates are typically denser and younger than continental plates, and they are constantly moving due to the process of plate tectonics. Subduction zones are often found at the boundaries where oceanic plates meet continental plates.
Either plates gets subducted which is usually the older plate.
At a convergent boundary where two oceanic plates meet, the denser plate will typically subduct below the less dense plate. The denser plate is usually the older, cooler, and more compacted of the two plates.
Zombie apocalypse.
When an oceanic to oceanic happens, two oceanic plates converge and one of the plates subducts into a trench. The subducted plate sinks down into the mantle and begins to melt. Molten rock from the plate rises toward the surface and forms a chain of volcanic islands, also called a volcanic island arc, behind the trench in the ocean.
When it is two continental plates, new oceanic crust is formed, and when this continues, more oceanic crust is formed between the plates.
Oceanic plates typically subduct beneath continental plates or other oceanic plates at subduction zones. The denser oceanic plate is forced beneath the less dense continental plate, leading to the formation of features such as deep ocean trenches, volcanic arcs, and earthquakes.