The ocean ridges push the old crust into a convergent boundary where it goes into a mantle convection current. The crust then melts in the convection current and is pushed out of the ocean ridge to restart the process again.
Convection ocean ridges are places where two plates are spreading apart, and magma from the mantle rises up, creating new ocean crust. A good example of this is the Mid-Atlantis ridge, where the Eurasian plate and the North American plates are pulling away from each other, creating volcanoes and earthquakes.
Subduction zones occur most often between continental plates and ocean plates. The denser, heavier ocean plate, when pushed up against the lighter continental plate, is forced back down into the Earth, where it is destroyed. This happens often in contact between ocean plates and continent plates. The Himilayas are actually a result of this type of subduction: as the Indian-Australian plate is forced under the Eurasian plate, the Eurasian plate is actually pushed up. Mt. Everest is rising, very slightly, every year as the Eurasian plate continues to be forced up.
Mid ocean ridges are the zone where oceanic crust is formed and subduction zones are the zones where it sinks down into the mantle, so one looks basically at the birthplace and graveyard of the oceanic crust in these zones.
Both zones are associated with forces acting upon the oceanic crust.
The mid ocean ridges are a zone of high topography (they are effectively a mountain chain) and this this topography and the continuous generation of new (still hot) crust in this area creates a pushing effect (known as the ridge push).
In the subduction zone, old and cool oceanic crust is subducted into the mantle. Cold oceanic crust has a density which exceeds that of the upper mantle so that the oceanic crust actively sinks into the mantle (this is known as slab pull).
In that way the ridge push helps subducting the crust via pushing it or alternatively the subduction pull helps creating new oceanic crust.
Volcanoes can be created at subduction zones from the downward movement of water filled oceanic crust into the mantle and the melting of the crust above it.
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Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
oceanic lithosphere sinks at subduction zones but not at mid ocean ridges because at subduction zones the oceanic lithosphere is subducted, or sinks, under another plate. Oceanic Lithosphere sinks at subduction zones which are usually at convergent boundaries, but at mid-ocean ridges the plates are actually separating not coming together
The Mid-Atlantic Ridge is found on the ocean floor in the middle of the Atlantic Ocean.
Divergent boundaries form ocean ridges.
Divergent plates or mid-ocean ridges
Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
(1)midocean spreading ridges, (2) subduction zones, and (3) transform faults.Normal fault, Reverse fault, and strike-slip fault
oceanic lithosphere sinks at subduction zones but not at mid ocean ridges because at subduction zones the oceanic lithosphere is subducted, or sinks, under another plate. Oceanic Lithosphere sinks at subduction zones which are usually at convergent boundaries, but at mid-ocean ridges the plates are actually separating not coming together
oceanic lithosphere sinks at subduction zones but not at mid ocean ridges because at subduction zones the oceanic lithosphere is subducted, or sinks, under another plate. Oceanic Lithosphere sinks at subduction zones which are usually at convergent boundaries, but at mid-ocean ridges the plates are actually separating not coming together
At transform faults or transform zones.
The Mid-Atlantic Ridge is found on the ocean floor in the middle of the Atlantic Ocean.
where boundaries are often found at ocean ridges.
Divergent boundaries form ocean ridges.
Divergent plates or mid-ocean ridges
Volcanoes are formed. Sorry, that's all I know
It is created at mid-oceanic ridges (divergent boundaries) and it is destroyed at subduction zones (convergent boundary between oceanic crust and continental crust).
hot spots, divergent plate boundaries, and convergent plate boundaries.