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The two scientists who provided supporting evidence for Alfred Wegener's theory of continental drift were Harry Hess and Robert S. Dietz. Hess contributed the concept of seafloor spreading, demonstrating that new oceanic crust forms at mid-ocean ridges, pushing continents apart. Dietz further supported this by showing how symmetrical patterns of magnetic stripes on either side of these ridges indicated that continents were moving away from these spreading centers. Together, their work helped solidify the foundation for the modern theory of plate tectonics.

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The year after Wegener died, Arthur Holmes published his idea that thermal convection in the earth's mantle could cause continents to move. Holmes also suggested that the continents didn't move but were "carried" by larger pieces of the earth's crust. The controversy quieted down and fell from prominence until the 1960s, when new evidence was brought to the fore. Discoveries of the Mid-Ocean Ridge and the work of Harry Hess and others led to the development of plate tectonics. Though not without problems, this theory has gained wide acceptance. It is the most complete theory of global dynamics yet, and its roots lie in the work of Alfred Wegener.


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