Defien Sea Floor Spreading

Seafloor spreading definition is the divergence at mid ocean ridges of the tectonic plates underlying the oceans that is due to upwelling from the earth s interior of magma which solidifies and adds to the spreading plates.

Defien sea floor spreading.

Spreading rate is the rate at which an ocean basin widens due to seafloor spreading. Seafloor spreading definition a process in which new ocean floor is created as molten material from the earth s mantle rises in margins between plates or ridges and spreads out. The oceanic crust is composed of rocks that move away from the ridge as new crust is being formed. In the theory of plate tectonics the process by which new oceanic crust is formed by the convective upwelling of magma at mid ocean ridges resulting in.

Seafloor spreading happens at the bottom of an ocean as tectonic plates move apart. 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. The mid ocean ridge is the region where new oceanic crust is created. Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.

The motivating force for seafloor spreading ridges is tectonic plate pull rather than magma pressure although there is typically significant magma activity at spreading ridges. 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 definition a process in which new ocean floor is created as molten material from the earth s mantle rises in margins between plates or ridges and spreads out. The seafloor moves and carries continents with it.

The process of sea floor spreading. Spreading rates determine if the ridge is fast intermediate or slow. Seafloor definition the solid surface underlying a sea or an ocean. At ridges in the middle of oceans new oceanic crust is created.

The formation of the new crust is due to the rising of the molten material magma from the mantle by convection current.