they will form a mountain
It gets pushed down under the lighter plate. This process is called subduction.
The Earth's crust gets recycled through a process called plate tectonics. This occurs when tectonic plates move and interact with each other, leading to subduction zones where one plate is forced beneath another. This process can cause the crust to melt and form magma, which can then rise to the surface through volcanic activity.
Denser oceanic crust is typically found where tectonic plates converge, such as subduction zones. Here, older and more dense oceanic crust is forced beneath another tectonic plate, leading to its submersion into the mantle and recycling within the Earth's interior.
The recycling center would be at subduction zones associated with areas of plate collisions, where older, colder, more dense oceanic crust is being drawn into the asthenosphere, the uppermost layer of the mantle.
The denser oceanic plate gets subducted because it is heavier and sinks beneath the less dense plate. This is due to differences in their composition and temperature. The subduction process plays a key role in the formation of features like deep ocean trenches and volcanic arcs.
Subduction.
when two oceanic plates collideSubduction zones form along convergent boundaries and can be thousands of kilometers long. Subduction zones allows one plate to slide beneath another plate, and enter into the mantle.
It gets pushed down under the lighter plate. This process is called subduction.
True. As tectonic plates are forced under another plate during subduction, earthquakes tend to occur at progressively shallower depths in the direction of the subduction zone. This is because the stress and pressure on the descending plate increase as it gets closer to the surface, resulting in more frequent and shallower earthquake activity.
The colder, more dense plate is the one that subducts in a collision between two plates. In an oceanic to oceanic plate collision it is the older of the two plates that will subduct due to its higher density. In an oceanic to continental plate collision, it's the oceanic plate that will subduct because of its higher density.
A geographical subduction zone is a fault line where two plates move towards each other. The more dense plate gets pushed under the other; this is called subduction.
a subduction boundry, this is where one plate gets pushed under the other. in this case the pacific plate is being pushed under the eurasion!
A subduction zone is an area of tectonic plate collision where the more dense plate subducts, or follows a path underneath, the less dense plate.A subduction zone is the place where oceanic plate margin is being pushed under a continental plate or a less dense oceanic plate. Have a look at the western side of South America (on the pacific coast), see the mountain ranges and volcanoes - these are just inside the edge of the continental plate and are a product of the subduction zone. As oceanic crust gets pushed under or over-ridden by the continental plate edge it melts and gives rise to the volcanoes. These zones also exist where one oceanic crust is pushed under another oceanic crust, the same volcanism results, but as it takes place at sea the result is the formation of underwater volcanoes.
Subduction Zones are usually known to be part of the Destructive Plate Boundary. The changes that occur in this boundary are: Oceanic crust moves towards the continental crust, but due to the weight of the oceanic crust, the oceanic crust sinks and gets destroyed. This forms deep sea trenches and island archs with volcanoes. As the oceanic crust is forced downwards, the increase in pressure can trigger earthquakes to strike... Basically, the two plates (oceanic and continental) are associated with subduction zones.... Hope this helped ^ ^
The Earth's crust gets recycled through a process called plate tectonics. This occurs when tectonic plates move and interact with each other, leading to subduction zones where one plate is forced beneath another. This process can cause the crust to melt and form magma, which can then rise to the surface through volcanic activity.
It gets very hot.
Denser oceanic crust is typically found where tectonic plates converge, such as subduction zones. Here, older and more dense oceanic crust is forced beneath another tectonic plate, leading to its submersion into the mantle and recycling within the Earth's interior.