Evidence That Prove Sea Floor Spareading

First samples of the deep ocean floor show that basaltic oceanic crust and overlying sediment become progressively younger as the mid ocean ridge is approached and the sediment cover is thinner near the ridge.

Evidence that prove sea floor spareading.

Paleomagnetism led the revival of the continental drift hypothesis and its transformation into theories of sea floor spreading and plate tectonics. Spreading rate is the rate at which an ocean basin widens due to seafloor spreading. Magnetic evidence for seafloor spreading explains how magnetic polarity frozen into seafloor basalts reveals evidence for the creation of new seafloor at mid ocean ridges. Tuzo wilson combined the continental drift and seafloor spreading hypotheses to propose the theory of plate tectonics.

Evidence of sea floor spreading harry hess s hypothesis about seafloor spreading had collected several pieces of evidence to support the theory. These age data also allow the rate of seafloor spreading to be determined and they show that rates. Eruptions of molten material magnetic stripes in the rock of the ocean floor and the ages of the rocks themselves. Abundant evidence supports the major contentions of the seafloor spreading theory.

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. Tuzo said that earth s crust or lithosphere was divided into large rigid pieces called plates. In 1965 a canadian geophysicist j. This evidence was from the investigations of the molten material seafloor drilling radiometric age dating and fossil ages and the magnetic stripes.

The regions that hold the unique record of earth s magnetic field lie along the mid ocean ridges where the sea floor is spreading. Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor. 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. Spreading rates determine if the ridge is fast intermediate or slow.

Several types of evidence supported hess s theory of sea floor spreading. This evidence led scientists to look again at wegener s hypothesis of continental drift. 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. Evidence for sea floor spreading.