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.
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
One of the midocean ridges is, but others are in other oceans, seas, and bays.
Mid-ocean ridges are not associated with subduction zones. They are divergent plate boundaries where tectonic plates are moving away from each other, leading to the formation of new oceanic crust. Subduction zones, on the other hand, are convergent plate boundaries where one tectonic plate is being forced beneath another.
Divergent boundaries form 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
At transform faults or transform zones.
No, subduction is not characteristic of diverging plate boundaries. Subduction occurs at converging plate boundaries where one tectonic plate is forced beneath another plate. Diverging plate boundaries are where tectonic plates move away from each other, such as at mid-ocean ridges.
Divergent boundaries are found along mid-ocean ridges, convergent boundaries are found at subduction zones and mountain ranges, and transform boundaries are found along fault lines like the San Andreas Fault in California.
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
One of the midocean ridges is, but others are in other oceans, seas, and bays.
divergent boundaries
Mid-ocean ridges are not associated with subduction zones. They are divergent plate boundaries where tectonic plates are moving away from each other, leading to the formation of new oceanic crust. Subduction zones, on the other hand, are convergent plate boundaries where one tectonic plate is being forced beneath another.
Divergent boundaries form ocean ridges.
mid-ocean ridges and subduction zones