Two plates move away from each other then hot rock from mantle below migrates up and fills void the hot rock cools and makes a new lithosphere.
Sea floor spreading forms where two plates.
These age data also allow the rate of seafloor spreading to be determined and they show that rates.
Mountains form from.
Seafloor spreading helps to explain continental drift in the theory of plate tectonics.
The two plates slip past each other.
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.
Plate boundary where two tectonic plates come together but the older and more dense oceanic crust subducts underneath the less dense younger oceanic crust oceanic crust is always more dense than continental crust so it will subduct underneath.
Subduction and sea floor spreading are processes that could alter the size and form of the ocean.
Between the two plates is a rift valley.
Seafloor spreading is what operates the system.
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.
The type of plate boundary and the type of crust found on each side of the boundary determines what sort of geologic activity will be found there.
1 data collected from.
Seafloor spreading theory that oceanic crust forms along submarine mountain zones known collectively as the mid ocean ridge system and spreads out laterally away from them.
Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.
The east pacific rise is a mid oceanic ridge a divergent tectonic plate boundary located along the floor of the pacific ocean it separates the pacific plate to the west from north to south the north american plate the rivera plate the cocos plate the nazca plate and the antarctic plate it runs south from the gulf of california in the salton sea basin in southern california to a point.
For instance the atlantic ocean is believed to be expanding because of its few trenches.
Plates move apart at mid ocean ridges where new seafloor forms.
2 10 describe two methods researchers use to measure relative plate motion.
A place where two plates slip past each other moving in opposite directions is known as a.
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.
The phenomenon is known today as plate tectonics.
Would form in the center of the older piece.
In sea floor spreading molten material rises from the mantle and erupts.
