The trenches catch most of the sediment from the plates that break up and sink deeper into the water. This causes the upper plates to grow.
When seafloor spreading happens, a rift forms at the bottom of a ocean and separates to form new rock. This is an example of a divergent plate boundary
Lava
It falls and break
The volcanic rock would be a mafic rock pushed up from the seafloor as the continents collided.
All three rock types could be formed in areas under the seas. Two types of rock are most likely to form on the seafloor, however. Sedimentary rock is formed on the seafloor where accumulations of sediments undergo lithification processes. Extrusive igneous rock can form on the seafloor when lava erupts on its surface.
The seafloor rocks vary in different places. Rock samples near ocean ridges are younger than rocks at deep sea trenches
When seafloor spreading happens, a rift forms at the bottom of a ocean and separates to form new rock. This is an example of a divergent plate boundary
Continental plates are massively granitic rock, oceanic plates massively basaltic rock, therefore continental rock is less dense than seafloor rock and has a different chemical and mineralogical composition.
An isochron is a line on a map that connects points that have the same age. An isochron map of the ocean floor supports the theory of seafloor spreading because it shows the older rock near the deep sea trenches and the younger rocks near ocean ridges.
Age of seafloor rock and sediment increases with distance from the oceanic ridges.
rock bottom
it turns into sediment
It turns into rock.
It will be an igneous rock
Lava
they are pushed down
erosion