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A convergent plate boundary, otherwise known as a destructive plate margin, forms volcanoes. This happens when -The subducting plate brings down silicates such as sand down with it. -Eventually, the plate melts but mixes with the silicates. This forms a more viscose but lighter magma -This rises because it is lighter until it reaches the moho, (the boundary between the lithosphere and the asthenosphere, (the plate and the stuff it floats own). This is the other plate. -It then breaks though, slowly rising to the surface. -It then erupts out of a volcano a few miles in to land. (This is the continental-oceanic process. The oceanic-oceanic, is slightly different).
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.
Subduction is a process that occurs when two oceanic plates pull apart
This is known as a subduction zone.
When the denser plate subducts (usually the oceanic crust) it gets pushed down into the hot asthenosphere and melts a little. this causes the magma created from the melting to rise up and shoot out of the earth's crust, forming a volcano.
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.
The oceanic plate must be more dense than the continental plate for this to happen.
Subduction
The oceanic plate will be subdued down into the mantle because it is denser. Or has more density*smiles* Hope I helped.
A convergent plate boundary, otherwise known as a destructive plate margin, forms volcanoes. This happens when -The subducting plate brings down silicates such as sand down with it. -Eventually, the plate melts but mixes with the silicates. This forms a more viscose but lighter magma -This rises because it is lighter until it reaches the moho, (the boundary between the lithosphere and the asthenosphere, (the plate and the stuff it floats own). This is the other plate. -It then breaks though, slowly rising to the surface. -It then erupts out of a volcano a few miles in to land. (This is the continental-oceanic process. The oceanic-oceanic, is slightly different).
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 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 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.