The vine matthews morley hypothesis also known as the morley vine matthews hypothesis was the first key scientific test of the seafloor spreading theory of continental drift and plate tectonics. The vine matthews morley hypothesis also known as the morley vine matthews hypothesis was the first key scientific test of the seafloor spreading theory of continental drift and plate tectonics its key impact was that it allowed the rates of plate motions at mid ocean ridges to be computed. According to hess seafloor was created at mid oceanic ridges by the convection of the earth s.
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