As the seafloor spreading axis moves along the margin thermal uplift produces a ridge.
Seafloor spreading evidence examples and explanations.
Spreading rates determine if the ridge is fast intermediate or slow.
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 evidence was from the investigations of the molten material seafloor drilling radiometric age dating and fossil ages and the magnetic stripes.
Spreading rate is the rate at which an ocean basin widens due to seafloor spreading.
Several types of evidence supported hess s theory of sea floor spreading.
Hess its major tenets gave great support to the theory of continental drift continental drift geological theory that the relative positions of the continents on the earth s surface have.
Around 250 million years ago the north poles were also different for the two continents the scientists looked again at the three possible explanations.
First proposed in the early 1960s by the american geologist harry h.
This evidence led scientists to look again at wegener s hypothesis of continental drift.
Eruptions of molten material magnetic stripes in the rock of the ocean floor and the ages of the rocks themselves.
A veritable legion of evidence supports the seafloor spreading hypothesis.
Evidence of sea floor spreading harry hess s hypothesis about seafloor spreading had collected several pieces of evidence to support the theory.
Plate tectonics theory dealing with the dynamics of earth s outer shell that revolutionized earth sciences by providing a uniform context for understanding mountain building processes volcanoes and earthquakes as well as the evolution of earth s surface and reconstructing its past continents and oceans.
Evidence for sea floor spreading.
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.
Molten rock erupts onto the seafloor there then cools and rifts away from the ridge on either side in a process known as seafloor spreading.
Studies conducted with thermal probes for example indicate that the heat flow through bottom sediments is generally comparable to that through the continents except over the mid ocean ridges where at some sites the heat flow measures three to four times the normal value.
A profound consequence of seafloor spreading is that new crust was and still is being continually created along the oceanic ridges.
Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.
