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Q: Which was the theory of Harry Hess?
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Who proposed the theory of seafloor spreading based on maps of the ocean floor?

The theory of seafloor spreading was proposed by Harry Hess, a geologist and Navy officer, in the early 1960s. He proposed that new oceanic crust is formed at mid-ocean ridges and then spreads outward. This theory helped to explain the mechanism behind continental drift and plate tectonics.


What supported Harry Hess theory?

Milk and your moms poo


What was the two discovery Harry Hess?

The Seafloor Spreading Theory


What was the theory Harry Hess proposed?

he proposed that mid-ocean ridges were areas where the floors of oceans had split apart


Who discovered Seafloor Spreading?

Henry H. hess


What did Harry Hess invent?

Harry Hammond Hess is not known for any invention. He was, however, one of the primary developers in the modern theory of plate tectonics.


Is it true that Harry Hess introduced the theory of continental drift?

yes


What evidence supports Harry Hess's theory?

Milk and your moms poo


Did harry hess find the mid-ocean ridge?

Yes, Harry Hess proposed the theory of seafloor spreading and the existence of mid-ocean ridges during the 1960s. His work significantly contributed to the development of the theory of plate tectonics.


Why did people believe Harry Hess and not believe Alfred Wegener?

Harry Hess proposed the theory of seafloor spreading, which provided physical evidence for the movement of the Earth's crust. Alfred Wegener proposed the theory of continental drift, which lacked a mechanism to explain how continents moved. Hess's theory had more scientific support and evidence, leading to greater acceptance by the scientific community.


How are Alfred Wegener and Harry Hess similar?

they both were associated with plate boundaries and continental drift. Harry Hess's theory proved Alfred's to be true.


When did harry hess propose seafloor spreading?

Harry Hess proposed the idea of seafloor spreading in the early 1960s, with his initial proposal being presented in 1960. This concept revolutionized our understanding of plate tectonics and the movement of the Earth's lithosphere.