New oceanic lithosphere forms as a result of continental drift.
New Oceanic lithosphere forms as a result of sea-floor spreading or continental drift.
no
A Mid-Ocean-Ridge develops leading to volcanism and the creation of new oceanic crust.
New lithosphere is constantly being produced at the oceanic ridges. Lithosphere is consumed at the subduction zones. A balance is maintained because older, denser proportions of oceanic lithosphere descend into the mantle at a rate equal to seafloor production.
Just as new oceanic crust forms at mid-ocean ridges, old oceanic crust is destroyed at subduction zones.
Seafloor Spreading.
Yes; at divergent/constructive boundaries, plates move apart and new oceanic lithosphere forms.
because stuff goes and hits some other stuff and.........BOOM..... oceanic lithosphere
seafloor spreading
no
A Mid-Ocean-Ridge develops leading to volcanism and the creation of new oceanic crust.
New lithosphere is constantly being produced at the oceanic ridges. Lithosphere is consumed at the subduction zones. A balance is maintained because older, denser proportions of oceanic lithosphere descend into the mantle at a rate equal to seafloor production.
Just as new oceanic crust forms at mid-ocean ridges, old oceanic crust is destroyed at subduction zones.
The subduction process
New oceanic lithosphere is constantly being produced at mid-ocean ridges and is recycled back to the mantle at subduction zones.
Seafloor Spreading.
As the lithosphere cools, asthenosphere's hot rocks freeze onto their undersides. So lithosphere becomes thicker. As time goes on or within the time period of 10 million years, it even becomes thicker than asthenosphere.
New oceanic crust is created at the mid-ocean ridges where rift volcanoes feed solidifying magma from the asthenosphere to both sides of the divergent plate boundaries. The mid-ocean ridge marks the line where heat from the Earth's interior is being carried to the surface by convection currents in the mantle. At the opposite end of the convection currents, colder, denser, and older oceanic crust is being drawn down into the asthenosphere, the birth to death of oceanic crust occurring in roughly 150 million year cycles.