Sea Floor Spreading Occurs

Subduction and sea floor spreading are processes that could alter the size and form of the ocean.

Sea floor spreading occurs.

Seafloor spreading helps explain continental drift in the theory of plate tectonics. The process of subduction and sea floor spreading can change the size and shape of the oceans. This idea played a pivotal role in the development of the theory of plate tectonics which revolutionized geologic thought during the last quarter of the 20th century. That is the time it takes for new rock to form at the mid ocean ridge move atoss the ocean and sink into a trench.

Sea floor spreading occurs at the divergent plate boundaries. Down the middle of underwater mountain ranges is a device that scientist use to map the ocean floor. Seafloor spreading theory that oceanic crust forms along submarine mountain zones and spreads out laterally away from them. Seafloor spreading is a process that occurs at mid ocean ridges where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge.

Molten material erups the central valley of mid ocean ridges. Seafloor spreading is a process that occurs at mid ocean ridges where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge. Because of these processes the ocean floor is renewed about every 200 million years. A deep ocean trench is an underwater.

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. Seafloor spreading is a process that occurs at mid ocean ridges where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge. Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor. For instance the atlantic ocean is believed to be expanding because of its few trenches.

Due to this continuous seafloor spreading occurs and makes atlantic ocean floor to be connected to other continental crust making the ocean gets wider over the time.