Seafloor Spreading Can Explain Magnetic Stripes Of The Ocean Floor

False the concept of seafloor spreading was supported by magnetic polarity stripes on the ocean floor.

Seafloor spreading can explain magnetic stripes of the ocean floor.

The theory of plate tectonics states that the lithosphere which is the earth s outer layer is divided up into a dozens of irregularly shaped plates. Harry hess s hypothesis about seafloor spreading had collected several pieces of evidence to support the theory. The discovery of magnetic stripes on the seafloor in the 1950s validated the plate tectonics theory for the geological community. Seafloor spreading processes create new oceanic crust at mid ocean ridges and destroy older crust at deep sea trenches.

Spreading rates determine if the ridge is fast intermediate or slow. The earth s magnetic field reverses in a regular pattern every few hundred thousand years. Several types of evidence supported hess s theory of sea floor spreading. Because of these processes the ocean floor is renewed about every 200 million years.

Magnetic polarity stripes give clues to seafloor ages and the importance of mid ocean ridges in the creation of oceanic crust. These two things were the magnetic striping on the ocean floor and the age of seafloor rocks. The magnetism of mid ocean ridges helped scientists first identify the process of seafloor spreading in the early 20th century. Such magnetic patterns led to recognition of the occurrence of sea floor spreading and they remain some of the strongest evidence for the theory of plate tectonics.

When the earth s magnetic field reverses a new stripe with the new polarity begins. This evidence was from the investigations of the molten material seafloor drilling radiometric age dating and fossil ages and the magnetic stripes. Evidence for sea floor spreading. That is the time it takes for new rock to form at the mid ocean ridge move atoss the ocean and sink into a trench.

Magnetic striping of the sea floor after mid ocean ridges and trenches were discovered more evidence was discovered that helped to support the theory that the continents had moved around. The figure below includes two images of the ocean floor. This evidence led scientists to look again at wegener s hypothesis of continental drift. Basalt the once molten rock that makes up most new oceanic crust is a fairly magnetic substance and scientists began using magnetometers to measure the magnetism of the ocean floor in the 1950s what they discovered was that the magnetism of the ocean floor around.

Eruptions of molten material magnetic stripes in the rock of the ocean floor and the ages of the rocks themselves. Spreading rate is the rate at which an ocean basin widens due to seafloor spreading. Evidence of sea floor spreading.