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Divergent Boundary :)
igneous rock
New ocean floor is created at mic-ocean ridges which are divergent plate boundaries.
Mid-ocean ridges and seafloor spreading are characteristics of oceanic diverging plates, plates that are moving away from each other.
Shallow focus earthquakes occur at the mid ocean ridges because the thin lithosphere found there is to weak to allow a large amount of strain to build up and cause larger earthquakes.
Mid-ocean ridges are located at undersea divergent plate boundaries.
At the mid-ocean ridges, a divergent plate boundary.
go to google and type mid ocean ridge, and there will be pictures of oceans with ridges!
The type of faulting that characterizes mid-ocean ridges is a transform fault. This type of faulting occurs because transform fault ridges stay in the same fixed location, thus the new ocean sea floor being created at the ridges is pushed away from the ridge.
divergent
Mid-ocean ridge basalt is the most common type of rock on earth. The entire surface of the ocean is made up of it. Mid-ocean ridges are the source of shallow, small-magnitude earthquakes.
Divergent Boundary :)
Divergent Boundary :)
igneous rock
New ocean floor is created at mic-ocean ridges which are divergent plate boundaries.
Mid-ocean ridges and seafloor spreading are characteristics of oceanic diverging plates, plates that are moving away from each other.
dark colored and igneous