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- W4242479968 abstract "TODAY MOST EARTH SCIENTISTS accept continental drift as a geological fact. Relative movements between continents on a time scale of 108 years are necessary to explain many geological observations. The remarkable similarity in shape between the west coast of Africa and the east coast of South America has been recognized for nearly as long as accurate maps of the Atlantic have been available; many have assumed that these continents once were connected. It is also accepted that the continents float on the mantle much like blocks of wood on water." @default.
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- W4242479968 date "1969-04-01" @default.
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- W4242479968 title "Continental drift" @default.
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- W4242479968 doi "https://doi.org/10.1063/1.3035524" @default.
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