The part of the plate that is subducting gets melted into magma and flows back into the mantle.
The edge of the that's being pushed downwards eventually reaches the molten lava under the crust, and melts.
It sinks (and partially melts causing volcanoes above it) deep into the mantle where it is warmed up again. It then rises in the mid oceanic ridges.
They are melted.
the materials melt
The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.
Ocean plates to be subducted into the mantle
Eventually the oceanic crust, along with the magnetically aligned minerals contained within, will be subducted into the mantle.
because oshieotic crust is under Mantle is thicker
The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.
The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.
The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.
Oceanic crust gets subducted into the mantle.
The colliding plate edges become crumpled to form a mountain range.
Or they get subducted and re-enter the mantle or they get obducted onto continent (the latter being called an ophiolite).
Older, colder, more dense oceanic crust is being subducted into the mantle.
No. They will either be subducted into the mantle or uplifted and/or exposed to erosion.
Ocean plates to be subducted into the mantle
The convection currents are a result of heat from the interior of the Earth. The rock of the upper mantle known as the asthenosphere is plastic-like but not molten. It acts like a conveyor belt, moving heat from Earth's interior upward, and cooled material downward in a big loop. New crust is created where mantle material reaches the surface at places called mid-ocean ridges. Older, colder oceanic crust is subducted and drawn into the mantle, completing the loop.
The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.
Convection currents occur as hot material expands and rises, and cool material contracts and sinks, much like a conveyor belt. It is new material from the Earth's center that rises and old material that sinks. The rising material pushes old material to the side, driving the lithosphere plates apart. The sinking material causes the plates to be pushed together.