Dietz and hess were among the small handful who really understood the broad implications of sea floor spreading.
Why is the sea floor spreading.
Subduction and sea floor spreading are processes that could alter the size and form of the ocean.
Using new data analysis techniques nasa scientists have confirmed the earth isn t expanding putting to rest years of rumors that the earth is growing.
Seafloor spreading is the mechanism by which new seafloor lithosphere is constantly being created at mid ocean ridges.
For instance the atlantic ocean is believed to be expanding because of its few trenches.
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.
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.
This theory introduced by harry hess.
Spreading rates determine if the ridge is fast intermediate or slow.
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.
Seafloor spreading is a geologic process where there is a gradual addition o.
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 occurs along mid ocean ridges large mountain ranges rising from the ocean floor.
If the earth s crust was expanding along the oceanic ridges hess reasoned it must be shrinking elsewhere.
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.
He suggested that new oceanic crust continuously spread away from the ridges in a conveyor belt like motion.
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.
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.
