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What was Harry Hess hypothesis called?
seafloor spreading
Building on the work of English geologist Arthur Holmes in the 1930s, Hess’ research ultimately resulted in a ground-breaking hypothesis that later would be called seafloor spreading. In 1959, he informally presented this hypothesis in a manuscript that was widely circulated.
What did Hess contribute to the theory of plate tectonics?
Hess explained that new crust was created at the Great Global Rift and was pushed under the continental crust about 300 million years later where it would melt and turn into magma. This motion also explained the formation of the guyots that were found at the bottom of the ocean.
What processes are involved in seafloor spreading?
Seafloor spreading occurs at divergent plate boundaries. As tectonic plates slowly move away from each other, heat from the mantle’s convection currents makes the crust more plastic and less dense. The less-dense material rises, often forming a mountain or elevated area of the seafloor. Eventually, the crust cracks.
What did Hess discover that was such a big surprise?
What Hess discovered was a big surprise. That enabled Hess to understand his ocean floor profiles in the Pacific. He realized that the Earth’s crust had been moving away on each side of oceanic ridges, down the Atlantic and Pacific oceans, that were long and volcanically active.
What did Harry Hammond Hess discover?
It was Hess who determined how oceanic mountain ranges, called mid-ocean ridges, are fundamental to the tectonic movement that results in the drift of continents.
What is the subject of the vine Matthews Morley hypothesis?
The Vine‐Matthews‐Morley (VMM) hypothesis states that, when ocean crust forms at a midocean ridge (i.e., a spreading center), the cooling crust becomes magnetized in the direction of Earth’s prevailing magnetic field as it cools below the Curie temperature of the magnetic minerals (Morley and Larochelle, 1964; Vine and …
What did Hess call his discovery?
He published ‘The History of Ocean Basins’ in 1962, in which he outlined a theory that could explain how the continents could actually drift. This theory later became known as ‘Sea Floor Spreading’.
Which concept is described in the theory proposed by Hess?
concept is described in the theory proposed by Hess is that Mid-ocean ridges are sites of seafloor spreading. Explanation: With time there is a change in the continental structure and the ocean surface and the sea floor.
What do you call the process that forms and moves new oceanic crust?
Seafloor spreading or Seafloor spread 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.
What is Harry Hess best known for?
Harry Hess was a geologist and Navy submarine commander during World War II. Part of his mission had been to study the deepest parts of the ocean floor. In 1946 he had discovered that hundreds of flat-topped mountains, perhaps sunken islands, shape the Pacific floor.
What did Vine and Matthews discover?
Vine and Matthews noticed there was a symmetrical pattern of magnetic stripes on either side of the mid ocean ridges. They published the idea in 1963 in a Nature paper called ‘Magnetic anomalies over oceanic ridges’.