Which Boundaries Is Sea Floor Created

Between the spreading segments the sides of the transform boundary rub together.

Which boundaries is sea floor created.

The impact of the colliding plates. What kind of plate boundary is forming between the. Convergent boundaries are formed wherever two plates move toward each other. Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.

When two plates come together it is known as a convergent boundary. At a divergent boundary mid oceanic ridges are created where sea floor spreading takes place. Boundary type movement types of crust involved sea floor created or destroyed. The result is a split in the crust called a fracture zone that extends across the seafloor far beyond the small transform that created it.

The mid atlantic ridge for instance separates the north american plate from the eurasian plate and the south american plate from the african plate the east pacific rise is a mid ocean ridge that runs through the eastern pacific ocean and separates the pacific plate from the north american. Sea floor spreading is the process in which new ocean floor is continually being formed as magma rises to the surface and hardens into rock. A divergent boundary occurs when two tectonic plates move away from each other. The divergent boundaries are the areas where plates are moving apart from one another.

Divergent boundaries are formed where two plates pull apart from each other the most famous example is the mid atlantic ridge where the north american and eurasian plates diverge. Tectonic process other processes earthquakes examples ocean ocean created sea floor spreading sub sea volcanism up to m 7 5 mid atlantic ridge east pacific rise divergent directly apart continent continent created continental rifting up to m 7 5 east african. The red sea has not yet completely split arabia from africa but a similar feature can be found on the other side of africa that has broken completely free. New crust is mainly created at plate boundaries in mid ocean where the sea floor is spreading older crust is destroyed near the edges of oceans where plates collide and one subducts dives below the other and melts.

The edges of the plates that make up the lithosphere are called boundaries or margins. But as soon as the seafloor spreads beyond the overlap the two sides stop rubbing and travel abreast. Seafloor spreading can stop during the process but if it continues to the point that the continent is completely severed then a new ocean basin is created. Where plates move apart new crustal material is formed from molten magma from below the earth s surface.

Because of this the youngest sea floor can be found along divergent boundaries such as the mid atlantic ocean ridge.