How Does Seafloor Spreading Help The Theory Of Continental Drift?

by | Last updated on January 24, 2024

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Seafloor spreading helps explain continental drift in the theory of plate tectonics. When oceanic plates diverge, tensional stress causes fractures to occur in the lithosphere . ... At a spreading center, basaltic magma rises up the fractures and cools on the ocean floor to form new seabed.

How does seafloor spreading affect the continents?

Eventually, geologists predict, seafloor spreading will completely separate the two continents —and join the Red and Mediterranean Seas. Mid-ocean ridges and seafloor spreading can also influence sea levels. As oceanic crust moves away from the shallow mid-ocean ridges, it cools and sinks as it becomes more dense.

How did seafloor spreading support continental drift quizlet?

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. Seafloor spreading helps explain continental drift in the theory of plate tectonics. ... Also that the continents are always slowly moving.

What supports the theory of seafloor spreading?

Abundant evidence supports the major contentions of the seafloor-spreading theory. 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.

What is the difference between continental drift seafloor spreading and plate tectonics?

Supporters of continental drift originally theorized that the continents moved (drifted) through unmoving oceans. Seafloor spreading proves that the ocean itself is a site of tectonic activity . Seafloor spreading is just one part of plate tectonics. Subduction is another.

What are 3 pieces of evidence that support seafloor spreading?

Several types of evidence from the oceans supported Hess’s theory of sea-floor spreading- evidence from molten material, magnetic stripes, and drilling samples .

What are the 3 evidences for seafloor spreading?

Harry Hess’s hypothesis about seafloor spreading had collected several pieces of evidence to support the theory. This evidence was from the investigations of the molten material, seafloor drilling, radiometric age dating and fossil ages, and the magnetic stripes .

What is the importance of seafloor spreading?

Seafloor spreading proves that the ocean itself is a site of tectonic activity . Seafloor spreading is just one part of plate tectonics. Subduction is another. Subduction happens where tectonic plates crash into each other instead of spreading apart.

What are the 4 evidence of continental drift?

They based their idea of continental drift on several lines of evidence: fit of the continents, paleoclimate indicators, truncated geologic features, and fossils .

What evidence did Alfred use?

He used fossil evidence , such as that of tropical plants found on the Arctic island of Spitzbergen. He found large-scale geographic features that matched, like the Appalachian Mountains in the United States and the Scottish Highlands, as well as rock strata in South Africa that matched those in Brazil.

What are the features of seafloor?

Features of the ocean include the continental shelf, slope, and rise . The ocean floor is called the abyssal plain

What is seafloor spreading and why is it important?

Today it refers to the processes creating new oceanic lithosphere

Who proposed the theory of seafloor spreading?

Harry Hess

What happens when the seafloor spreads?

Seafloor spreading

Is the Earth’s diameter getting bigger because of seafloor spreading?

New crust is continually being pushed away from divergent boundaries (where sea-floor spreading occurs), increasing Earth’s surface. But the Earth isn’t getting any bigger .

What are the steps in the process of seafloor spreading?

  1. Magma comes out of the rift valley.
  2. Magma cools to rock and hardens.
  3. Rock is pushed away as new rock is formed at MOR.
  4. Oceanic crust and continental crust meet at the trench.
  5. Oceanic crust bends down under the continental crust.
  6. Gravity pulls rock towards mantle.
  7. Rock melts to mantle.
Emily Lee
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Emily Lee
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