The mantle is below the plates.
As an oceanic plate sinks into the mantle at a convergent boundary it causes rocks to melt. Some of the newly formed magma will migrate upward to volcanoes, that have formed along the convergent boundaries, and erupt.
The boundaries between two colliding plates is called a convergent boundary. Earthquakes and volcanoes are common near convergent boundaries, a result of pressure, friction, and plate material melting in the mantle.
Volcanic mountains over hot spots in the mantle. Fault-block
They mark the boundaries of differing layers of the Earth. The Moho marks the boundary between the crust and the mantle, whereas the Gutenberg discontinuity marks the boundary between the mantle and outer core.
At this type of convergent boundary the oceanic plate will be subducted, or sink into the mantle underneath the continental plate. Volcanoes often form near these boundaries.
This occurs at a convergent plate boundary and is known as subduction.
Convergent boundary+oceanic plate=subduction because the oceanic plate is more dense causing it to subduct down back to the mantle.
As an oceanic plate sinks into the mantle at a convergent boundary it causes rocks to melt. Some of the newly formed magma will migrate upward to volcanoes, that have formed along the convergent boundaries, and erupt.
The boundaries between two colliding plates is called a convergent boundary. Earthquakes and volcanoes are common near convergent boundaries, a result of pressure, friction, and plate material melting in the mantle.
The oceanic plate will be subdued down into the mantle because it is denser. Or has more density*smiles* Hope I helped.
Volcanic mountains over hot spots in the mantle. Fault-block
They mark the boundaries of differing layers of the Earth. The Moho marks the boundary between the crust and the mantle, whereas the Gutenberg discontinuity marks the boundary between the mantle and outer core.
The boundary between the mantle and the core is called the core-mantle boundary and also The Gutenberg Discontinuity which marks the upper boundary of the D'' (D Double Prime) layer.
The boundary of mantle and core are called Gutenberg Discontinuity
It is folded and uplifted, or subducted into the mantle, depending on the type of convergent boundary.
convergent boundary
At this type of convergent boundary the oceanic plate will be subducted, or sink into the mantle underneath the continental plate. Volcanoes often form near these boundaries.