Rock moving away from a mid-ocean ridge is replaces by more oceanic crust.
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
continental crust.
It is a process called ridge push.
Cooling as rock moves away from the ridge crest causes the rock to become increasingly rigid.
friction - convection currents in the mantle drag the plates away from the hot rising zone below the ridgegravity - gravity pulls down on the cold dense plate being subducted under the continent, dragging the plate away from the ridge
No. The rock cools down as it moves away and sinks deeper.
True.
yes
They increase in age and density, and decrease in temperature.
The mid-ocean ridge is almost in all of the oceans
they are related because they all have to do with the oceanic lithosphere.The convection causes the lithosphere to move sideways and away from the midocean ridges.The ridge push makes the oceanic lithosphere slide downhill under the force of gravity. The slab pull:the old lithosphere is denser than asthenosphere so, the edge of the tectonic plates that contains oceanic lithosphere sinks and plls the rest of the tectonic plate.
cuz rocks come up from the ridge and create land by the ridge