A is called a subduction zone, where an oceanic plate converges with another tectonic plate, typically a continental plate, and is forced down into the asthenosphere. This process can lead to the formation of deep ocean trenches and volcanic arcs. The intense pressure and heat in the asthenosphere can cause the subducting plate to partially melt, contributing to magma formation and volcanic activity. Subduction zones are key areas for understanding plate tectonics and associated geological phenomena.
It is formed by a convergent boundary of an oceanic plate and continental plate when they hit each other and goes down into the asthenosphere thus making the magma to rise above the earth's surface making a volcano.Then it solidifies and therefore it makes a volcano island.
When an oceanic plate moves under a continental plate, a subduction zone is formed. The oceanic plate is forced down into the mantle, where it melts and creates magma. This magma can then rise to the surface, causing volcanic activity on the continental plate.
When an oceanic plate goes under a continental plate in a process called subduction, the oceanic plate is forced down into the mantle due to its higher density. This creates a subduction zone where the oceanic plate melts and forms magma, leading to volcanic activity. The continental plate is usually uplifted, creating mountain ranges.
The process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at a convergent plate boundary is called subduction. This occurs because oceanic crust is denser than the underlying asthenosphere, causing it to be pulled down into the mantle. Subduction zones are associated with the formation of volcanic arcs and deep-sea trenches.
This is known as a subduction zone.
the oceanic crust slides down and burns in the mantle and forms a volcano
a region where oceanic plates sink down into the asthenosphere is called a subduction zone.
A subduction zone is a region where oceanic plates sink down into the asthenosphere beneath another plate, such as at convergent plate boundaries. This process can lead to the formation of deep oceanic trenches, volcanic arcs, and earthquakes.
Subduction
The oceanic plate will be subdued down into the mantle because it is denser. Or has more density*smiles* Hope I helped.
when oceanic crust and continental crust collide, the oceanic crust sinks down beneath the continental crust. this is called subduction.
The oceanic crust consists of heavier rock, mostly Basalt, so that if a oceanic plate collides with a continental plate the oceanic plate will be forced down below the continental plate, forming island arcs.continental plates are thicker than oceanic plates.
The plate with cooler, denser crust sinks under the other plate, forming a trench. There, the oceanic crust sinks down back into the mantle.
The plate with cooler, denser crust sinks under the other plate, forming a trench. There, the oceanic crust sinks down back into the mantle.
It is formed by a convergent boundary of an oceanic plate and continental plate when they hit each other and goes down into the asthenosphere thus making the magma to rise above the earth's surface making a volcano.Then it solidifies and therefore it makes a volcano island.
When an oceanic plate moves under a continental plate, a subduction zone is formed. The oceanic plate is forced down into the mantle, where it melts and creates magma. This magma can then rise to the surface, causing volcanic activity on the continental plate.
When an oceanic plate goes under a continental plate in a process called subduction, the oceanic plate is forced down into the mantle due to its higher density. This creates a subduction zone where the oceanic plate melts and forms magma, leading to volcanic activity. The continental plate is usually uplifted, creating mountain ranges.