Spreading rates determine if the ridge is fast intermediate or slow.
Sea floor spreading is responsible for what.
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.
With the discovery of plate tectonics and the mapping of the earth.
Subduction and sea floor spreading are processes that could alter the size and form of the ocean.
The process of subduction and sea floor spreading can change the size and shape of the oceans.
Seafloor spreading is the continuous process of forming new igneous rock at midocean ridges by injection of magma that forms new seafloor.
The rate at which new oceanic lithosphere is added to each tectonic plate on either side of a mid ocean ridge is the spreading half rate and is equal to half of the spreading rate.
Because of these processes the ocean floor is renewed about every 200 million years.
This can result in an ever widening seafloor at the.
Seafloor spreading theory that oceanic crust forms along submarine mountain zones and spreads out laterally away from them.
Spreading rate is the rate at which an ocean basin widens due to seafloor spreading.
These age data also allow the rate of seafloor spreading to be determined and they show that rates.
Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.
Hess proposes sea floor spreading 1960.
For instance the atlantic ocean is believed to be expanding because of its few trenches.
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.
Harry hess argues that the continents had once been one and have drifted apart.
The following features are shown at example depths to scale though each feature has a considerable range at which it may occur.
The process is continuous because forces cause opposite sides of the midocean ridge to constantly move apart making new room for the process to repeat.
This seafloor spreading hypothesis had been proposed a few years earlier by harry hess a petrologist at princeton university and robert dietz an oceanographer in the us coast and geodetic survey the federal department that made maps of the oceans and us coastlines.
This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level.
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.
Hess went on to say that as the ocean crust spreads and cools over millions.
