The process of sea floor spreading created the lithosphere under the atlantic ocean.
Se floor spreading.
The continents bordering the atlantic ocean for example are believed to be moving away from the mid atlantic ridge at a rate of 1 2 cm 0 4 0 8 inch per year thus increasing.
The process of sea floor spreading.
The formation of the new crust is due to the rising of the molten material magma from the mantle by convection current.
Molten mantle materials continually rise to fill the cracks formed as.
Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.
The mid ocean ridge is the region where new oceanic crust is created.
Igneous rocks rise along conduits from the mantle giving rise to volcanic activity in a narrow band along the mid ocean ridges as these cool the basaltic lavas and dykes form the upper part of the oceanic crust and the underlying magma chamber solidifies to.
As north america and south america moved away from europe and africa the resulting crack was filled by mantle material which cooled and formed new lithosphere.
That is it explains why the age thickness and density of the oceanic crust increases with distance from the mid oceanic ridge.
This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level.
This spreading creates a successively younger ocean floor and the flow of material is thought to bring about the migration or drifting apart of the continents.
Spreading rate is the rate at which an ocean basin widens due to seafloor spreading.
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.
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 process continues today.
Spreading rates determine if the ridge is fast intermediate or slow.
The theory of sea floor spreading states that new oceanic crust is being formed continuously at mid oceanic ridges while the older rocks move away from the ridge.
Sea floor spreading the theory that the ocean floor is created at the spreading accretionary plate margins within the ocean basins.
