the colder,oceanic plate sinks?!?!
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.
When two plates carrying oceanic crusts meet at a trench, one plate typically subducts beneath the other due to its higher density. This process can generate volcanic activity, earthquakes, and the formation of deep-sea trenches and volcanic island arcs.
oceanic convergence is when two oceanic plates subduct beneath one another.
Oceanic plates are denser and thinner, found beneath the oceans, while continental plates are thicker and less dense, making up the Earth's landmasses. These two types of tectonic plates interact at boundaries, influencing processes like earthquakes and volcanic eruptions.
an earth quake happens when two plates meet
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 it is two continental plates, new oceanic crust is formed, and when this continues, more oceanic crust is formed between the plates.
volcanic mountains
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 two plates carrying oceanic crusts meet at a trench, one plate typically subducts beneath the other due to its higher density. This process can generate volcanic activity, earthquakes, and the formation of deep-sea trenches and volcanic island arcs.
Places, where plates meet, are called plate boundaries. There are seven significant plates along with countless minor plates. You can see that a plate can be made of both oceanic crust and continental crust. Interactions between the plates change our planet.
No subduction doesn't take place when two oceanic crust meet. When two oceanic crusts meet, it is called a divergent boundary. Crustal features vary such as one like mid-ocean rdges. Subducting takes place when an OCEANIC and CONTINENTAL plate meet not when two oceanic plates meet.
The younger of the two plates, because it is less dense,* will ride over the edge of the older plate.
If the plates are moving toward each other, the more dense oceanic plate will subduct underneath the less dense continental plate. Mountain ranges and volcanism may result as the water saturated subducting oceanic crust creates molten rock which attempts to rise to the surface.
The two types of tectonic plates are continental and oceanic.
oceanic convergence is when two oceanic plates subduct beneath one another.