Sea Floor Spreading Article And Questions

The process of sea floor spreading the mid ocean ridge is the region where new oceanic crust is created.

Sea floor spreading article and questions.

The rate of seafloor spreading is approximately every 10 years. Sea floor spreading answer key. The mid atlantic ridge for instance separates the north american plate from the eurasian plate and the south american plate from the african plate. A 3 inches b 30 meters c 30 inches d 3 cm e 30 cm.

As the ocean seafloor spreads the newly formed floor will adapt a specific magnetic signature according to the earth s magnetic pole at that time. Seafloor spreading theory that oceanic crust forms along submarine mountain zones and spreads out laterally away from them. 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 plate the cocos plate the nazca plate and the antarctic plate. Seafloor spreading is happening.

As upwelling of magma continues the plates continue to diverge a process known as seafloor spreading samples collected from the ocean floor show that the age of oceanic crust increases with distance from the spreading centre important evidence in favour of this process. Sea floor spreading occurs at the divergent plate boundaries. 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. The oceanic crust is composed of rocks that move away from the ridge as new crust is being formed.

Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor. As years pass lateral segments of seafloor will thus share the same. Swbat create a graph modeling the process of sea floor spreading in continental drift and rock formation big idea in this lesson students construct a graphical model of the ocean floor the atlantic ocean describing its physical features identifying its plate motion and associated characteristics and diagraming its magnetic polarity. This is a mid ocean ridge.

It is an underwater mountain range that forms when magma pushes up on the crust at a divergent boundary. The formation of the new crust is due to the rising of the molten material magma from the mantle by convection current.