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  2. Harry Hammond Hess - Wikipedia

    en.wikipedia.org/wiki/Harry_Hammond_Hess

    Harry Hammond Hess (May 24, 1906 – August 25, 1969) was an American geologist and a United States Navy officer in World War II who is considered one of the "founding fathers" of the unifying theory of plate tectonics.

  3. Vine–Matthews–Morley hypothesis - Wikipedia

    en.wikipedia.org/wiki/Vine–Matthews–Morley...

    Harry Hess proposed the seafloor spreading hypothesis in 1960 (published in 1962 [1]); the term "spreading of the seafloor" was introduced by geophysicist Robert S. Dietz in 1961. [2] According to Hess, seafloor was created at mid-oceanic ridges by the convection of the Earth's mantle, pushing and spreading the older crust away from the ridge. [3]

  4. Seafloor spreading - Wikipedia

    en.wikipedia.org/wiki/Seafloor_spreading

    Hess' theory was that new seafloor is formed when magma is forced upward toward the surface at a mid-ocean ridge. If spreading continues past the incipient stage described above, two of the rift arms will open while the third arm stops opening and becomes a 'failed rift' or aulacogen. As the two active rifts continue to open, eventually the ...

  5. Robert S. Dietz - Wikipedia

    en.wikipedia.org/wiki/Robert_S._Dietz

    Robert Sinclair Dietz (September 14, 1914 – May 19, 1995) was an American scientist with the United States Coast and Geodetic Survey.Dietz, born in Westfield, New Jersey, [1] was a marine geologist, geophysicist and oceanographer who conducted pioneering research along with Harry Hammond Hess concerning seafloor spreading, published as early as 1960–1961.

  6. Geomagnetic reversal - Wikipedia

    en.wikipedia.org/wiki/Geomagnetic_reversal

    In 1963, Frederick Vine and Drummond Matthews provided a simple explanation by combining the seafloor spreading theory of Harry Hess with the known time scale of reversals: sea floor rock is magnetized in the direction of the field when it is formed.

  7. Glomar Challenger - Wikipedia

    en.wikipedia.org/wiki/Glomar_Challenger

    The Glomar Challenger was built to help Harry Hess test the theory of seafloor spreading, which predicts that the age of rock samples increases with distance from the mid-ocean ridge. Accomplishments [ edit ]

  8. Timeline of the development of tectonophysics (after 1952)

    en.wikipedia.org/wiki/Timeline_of_the...

    With the theory of thrusting, nappes, thrust faults and subductions. The "Princeton University" group around H. H. Hess: Felix Andries Vening Meinesz, Harry Hammond Hess, John Tuzo Wilson, W. Jason Morgan and Frederick Vine. Overview of plate tectonics in: Kearey, Klepeis & Vine 2009.

  9. Frederick Vine - Wikipedia

    en.wikipedia.org/wiki/Frederick_Vine

    Frederick John Vine FRS (17 June 1939 – 21 June 2024) was an English marine geologist and geophysicist.He made key contributions to the theory of plate tectonics, helping to show that the seafloor spreads from mid-ocean ridges with a symmetrical pattern of magnetic reversals in the basalt rocks on either side.